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其他人还在看Distribution-of-subsurface-fluid-flow-systems-in-the-SW-Barents-Sea_2013
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Warehousesupervisor和warehouseproductdistributi仓库主管,仓库发货小组谁看过《恐怖洞》这部电影?请进来一下Harring...DanielBrockleb...索拉?伯奇……LizDun...…l影片类型:犯罪恐怖惊悚时长:102分钟首映:日英国发行:SevillePicturesPathéDistributi...A...distr是什么意思这是个描述文件答：可能是Distribution的缩写=发报Distribution-of-subsurface-fluid-flow-systems-in-the-SW-Barents-Sea_2013(图6)Distribution-of-subsurface-fluid-flow-systems-in-the-SW-Barents-Sea_2013(图8)Distribution-of-subsurface-fluid-flow-systems-in-the-SW-Barents-Sea_2013(图10)Distribution-of-subsurface-fluid-flow-systems-in-the-SW-Barents-Sea_2013(图13)Distribution-of-subsurface-fluid-flow-systems-in-the-SW-Barents-Sea_2013(图25)Distribution-of-subsurface-fluid-flow-systems-in-the-SW-Barents-Sea_2013(图27)
MarineandPetroleumGeology43(R软件的fitdistr函数问：my.est&-fitdistr(mydata,'beta',start=list(shape1=1,shape2=3))中sta...答：看看帮助文件：?fit防抓取，好心游戏网提供内容，请查看原文。ContentslistsavailableatSciVerseScienceDirectdistrbutedby:法文里是什么意思答：第三天让不特定扮演.防抓取，好心游戏网提供内容，请查看原文。MarineandPetroleumGeology精彩内容，尽在百度攻略：distrbutions是什么意思答：distributions[英][dɪstrɪb'ju:ʃnz][美][dɪstrɪb'ju:ʃnz]防抓取，好心游戏网提供内容，请查看原文。journalhomepage:/locate/marpdistrit与area和territory的区别答：district表达地区的意思时候是表达行政区划的意思；area表达地区区域的时候，表示的是地理概念的划分；territory则直接表示领地、领土防抓取，好心游戏网提供内容，请查看原文。etgeo精彩内容，尽在百度攻略：distractive和distracting的区别是什么？能否...答：一个形容词一个动词你说什么区别FlowersaroundtheheadisalsoverydistractiveDon'tdi防抓取，好心游戏网提供内容，请查看原文。Distributionofsubsurface?uid-?owsystemsintheSWBarentsSea苹果4通用里面多了个描述文件IOSEnterpriseDistr...答：1、IOSEnterpriseDistr是给苹果发送报告的配置描述文件。iphone描述文件是由iPhone配置实用工具生成的防抓取，好心游戏网提供内容，请查看原文。SunilVadakkepuliyambattaa,*,StefanBünza,JürgenMienerta,ShyamChandbmicrosoftvisualc++2012Redistrbutabie(x64)是...问：microsoftvisualc++2012Redistrbutabie(x64)是什么.，能删吗？答：不防抓取，好心游戏网提供内容，请查看原文。ab精彩内容，尽在百度攻略：什么是accumulationdistrbution答：accumulationdistrbution累积分布accumulation[英][əˌkju:mjə'le&#防抓取，好心游戏网提供内容，请查看原文。DepartmentofGeology,UniversityofTroms?,Dramsveien-201,9037Troms?,NorwayGeologicalSurveyofNorway(NGU),P.O.Box6315Sluppen,7491Trondheim,Norway防抓取，好心游戏网提供内容，请查看原文。articleinfo一星期前处个王者荣耀cp，加了微信一看，还挺好看。两个人发展感情很快，每天早安晚安，后来一起玩了游戏，我惊奇的发现，这个姑娘是真能bb啊，要是说玩的不好说几句队友，很正常，她会把全部说话开开，一个劲嘲防抓取，好心游戏网提供内容，请查看原文。Articlehistory:精彩内容，尽在百度攻略：玩了5年的起凡，不知道有没有人知道这个游戏。当时我还是小学的时候就比较火了（我08年6年级）。初一才开始到这个游戏。那个时候全班的男生百分之50都玩起凡。每天下课就聚在一起聊游戏。什么昨天我拿了两个m防抓取，好心游戏网提供内容，请查看原文。Received28July2012Receivedinrevisedform28January2013首先是你自己把自己玩累了，我就是把它当游戏玩，本来就是娱乐，当自己过于执着一段代码，而不是娱乐，交友，怎么都会累。我就是仅仅当做娱乐，每天两小时，刷刷世界，打打战场等等。其次魔兽是退步好多，但是我敢说防抓取，好心游戏网提供内容，请查看原文。Accepted1February2013上面提到的有认识的，也有不认识的。我就挑我知道的几个人来说说吧。小时候大约在上小学的时候，被同学带进游戏厅，从此接触到了拳皇，虽然至今仍然是个拳皇菜鸟但是对于拳皇高手一直处于45°仰望的感觉。前几年一防抓取，好心游戏网提供内容，请查看原文。Availableonline26February2013Keywords:Fluid?owGaschimneysGashydratesBarentsSeaSeismic精彩内容，尽在百度攻略：我觉得应该是李白第一，露娜第二，貂蝉第三把。李白是新买的，买完了立马配了一个千年之狐，感觉帅炸了，赶紧去秀，我已经预见到我就是下一个剑仙，我仿佛看到了我刷大抢龙拿五杀了，结果――0-5。嗯？我的打开方式不对(?°?°?)。再来一局――0-8，啊嘞=????(???*)，我还就不信了――0-12。啊啊啊根本就是骗我??(??￣??￣?)????貂蝉呢，真的很好看啊，好漂亮的感觉，而且好多女主播小姐姐防抓取，好心游戏网提供内容，请查看原文。abstract九年老玩家了，中间也穿插着玩过codol，前段时间还买了csgo（本人现在在日本留学，所以没考虑csgo国服）发现并不是我想象中的cs了，遂放弃。cf一直没断过，当然钱也没有少花，既然每天都要玩游戏，防抓取，好心游戏网提供内容，请查看原文。TheSWBarentsSeaisalargehydrocarbon-proneepi-continentalSeaoftheNorwegianArcticregion.Asigni?cantportionofthehydrocarbongasesgeneratedindeepsourcerockshasleakedormigratedintotheshallowsubsurfaceandisnowtrappedingashydrateandshallowgasreservoirs.Theevolutionofsedimentarybasinsofthisregionhascontrolledtheleakageofthese?uidsthroughmarinesediments.Understandingthedistributionofvarious?uid-?owsystemsmayenhanceourknowledgeoftheevo-lutionofdifferentbasinsintheSWBarentsSeaandcouldhelp?ndpotentialtargetsforfuturehydro-carbonexploration.Weanalyzeapproximately30002Dmulti-channelseismicpro?lesanddatafrom60wellscoveringtheentireSWBarentsSea,toidentifyandclassify?uid-?owfeatures,andstudytheirrelationshiptotectonicelementsandgeologicalhistory.Gaschimneysarethemostabundantfeatureamongvariousother?uid-?owfeaturessuchas?uidleakagealongfaultsandfractures,seepagepipes,andhighamplitudeanomaliespotentiallyindicatingtrapped?uids.Large?uid-?owfeatures,coveringareasaslargeas600km2,occurclosetoknownhydrocarbon?eldssuchasSn?hvit,Skrugard,andHavis.The?uid-?owfeaturesoccurabovemajordeep-seatedfaultsintheareasuggestingacloserelationtoit.Thenumberof?uid-?owfeaturesinthewesternpartofthestudyareaissigni?cantlyhigherthanintheeasternpart.Theamountofneterosioninthestudyareashowsnodirectcontroloverthedistributionof?uid-?owfeatures,suggestingthatthefaultsanddistributionofmaturesourcerockscontrolthe?uid?ow.Thestrongcorrelationbetweenthelocationsof?uid-?owfeaturesandstructuralelementsin-dicatesthatextensionaltectonics,upliftandglaciationscouldhaveplayedmajorrolesinthetimingandactivityofthe?uidleakage,althougherosionmighthavehadanaddedeffect.不会啊，我媳妇有时候安慰我还会送我皮肤呢。玩游戏嘛，每个人理解不一样。有的人觉得浪费，有的人觉得划算不贵，我觉得在能接受的范围里面都是可以的。其实这里面最耗钱的是水晶和符文，其余的不算贵。不过这游戏最舒服的就是带领队友获得胜利，不坑才是硬道理！最后来一波符文和限定皮肤^_^有你们想要的嘛^_^防抓取，好心游戏网提供内容，请查看原文。ó2013ElsevierLtd.Allrightsreserved.精彩内容，尽在百度攻略：我最后悔的是李白。。。哈哈手残个人觉得这些英雄容易买了后悔王者荣耀的英雄很多，但是新手就那么几个，虽然各种活动看上去能领的福利不少，但是能换成英雄的并不多，不是土豪的话，基本上一个月也就能搞1,2个英防抓取，好心游戏网提供内容，请查看原文。1.Introduction今天我要说的是关于本人的一个故事，一个关于《魔兽世界》JJC的故事个人认为魔兽世界PVP做的算是非常平衡了，首先天赋百花齐放，百家争鸣。部落最良心的地方就是不会出现土豪吊打潘康恼庵智榭龀鱿郑灰闶址雷ト。眯挠蜗吠峁┠谌荩氩榭丛摹Thevertical?owof?uidsthroughmarinesedimentsisawidespreadanddynamicgeologicalprocessthatoccursonpassiveandactivecontinentalmarginsworldwide.Fluidmigrationisassociatedwithexcesspore-?uidpressure,andisattributedtotemporallyandspatiallyvaryingprocesses,suchasrapidsedimentloading(e.g.DuganandFlemings,2000),upliftanderosion(e.g.DoréandJensen,1996),dissociationofgashydrate(e.g.Mienertetal.,2005),polygonalfaulting(e.g.Cartwrightetal.,2007),andhydrocarbongenerationandleakagefromdeepandshallowsourcerocksandreservoirs(e.g.Heggland,1998;SolheimandElverh?i,1985;HovlandandJudd,1988).Presenceofshallowgasaccumu-lationsassociatedwith?uidleakageareofinterestforseveralreasons:(1)Shallowgasaccumulationsmayreducetheshear小伙苦战195分钟获胜，后台却没有战绩，找客服理论无果只好以跳楼相逼。很多玩家放弃LOL转战王者荣耀，就是因为手机游戏时间短，一把只要十几二十分钟。而今天要说了这位玩家足足玩了195分钟王者荣耀，手机都要炸了。坚持打了195分钟，还不就是为了一个输赢？熬来熬去敌方终于坚持不住投降了，己方胜利但是却没有比赛记录，小伙子直接崩溃了，当场就想跳楼。从上图就可以看到这名玩家使用吕布打比赛，和敌方一共进行了195分钟的比赛，人头比高达155比72，因为两边都有黄忠，所以谁都攻不进谁最后敌方终于忍不住投降，己方苦战3个小时的比赛终于结束了，当最终的战绩竟然找不到了，小伙子气的不行，只好找客服问清楚。客服都防抓取，好心游戏网提供内容，请查看原文。*Correspondingauthor.Tel.:t.精彩内容，尽在百度攻略：《迷你世界》抄袭《Minecraft》是事实，有买《Minecraft》的版权的话，为什么《迷你世界》官方至今没把版权证明拿出来？《迷你世界》的皮肤人设极渣，还收费！艹！那么渣的皮肤也收费！《迷你世界防抓取，好心游戏网提供内容，请查看原文。E-mailaddress:sunil.vadakkepuliyambatta@uit.no(S.wot属于比较冷门的类型，但好制作比较精良，虽然根据游戏性的需求做了点妥协，但还是有一定的真实度的，但“黄金五九”之类的做法还是有点反胃。毕竟wot的题材和操作门槛没办法让绝大部分人适应（虽然已经很简防抓取，好心游戏网提供内容，请查看原文。精彩内容，尽在百度攻略：1、一个连补刀都不用的游戏！王者相对lol来说却是简单的多，甚至站在旁边死掉的兵都会给你加钱，所以lol的玩家就觉得这是一个弱智的游戏，但是玩游戏不是为了开心吗？又不要打职业，娱乐就好！2、嫉妒心理可防抓取，好心游戏网提供内容，请查看原文。Vadakkepuliyambatta)./$eseefrontmatteró2013ElsevierLtd.Allrightsreserved.http://dx.doi.org/10.1016/j.marpetgeo.我遇到最尴尬的一件事就是差点失去了我的第一次。当时正在包夜，一个女的从我身边走过，看着她火辣的身材加上黑丝皮裙就没忍住一直盯着看，想看她做哪台机，谁知她突然转头和我对视五秒钟，然后问我看什么。我鬼使神差的来一句看你好看，结果她竟然走了过来和我攀谈起来。接着就顺理成章的去开了房，正要办事的时候发现酒店没有套让我下来买，我下楼被冷风一吹突然冷静了下来，最后没敢在上去。跑回家睡觉了，白白浪费了我的包夜钱防抓取，好心游戏网提供内容，请查看原文。strengthofsediments,andposeahazardtohydrocarbonexplora-tionanddevelopment(Andreassenetal.,2007a),(2)theoccur-renceofshallowgasandindicationsof?uid?owunderlyingitmaypointtowarddeeperprospectivereservoirs(e.g.Heggland,1998)and(3)shallowgasaccumulationscouldbeofcommercialinterestinthefuture(Carstens,2005).早在去年，新年后不再破解游戏和转载破解资源，三大妈全面转型，要发展成为集卖正版，出攻略的综合性网站。此事件起因，是因一家日本公司发给三大妈的警告信（函）引起，具体过程是三大妈破解（转载）了《三国志13》这款所谓的3A大作，#(喷)#(滑稽)这破游戏谁玩谁知道，这里不是我为三大妈说话，只因为这破游戏国区390RMB？就是190，都不会有几个人买的烂游戏，不知道光荣哪来的勇气定价如此高，今后光荣游戏一生黑。因为此事，三大妈迫于压力，才决定不再出破解资源，这无疑是伸手党的晴天霹雳，寒冬要来了，现在已经可以预见，就算是其它网站暂时没事，那也只是短期，今后，将不会有破解游戏玩了。有一点很悲哀，三国演义是防抓取，好心游戏网提供内容，请查看原文。Verticalmigrationofgasthroughsubsurfacestratacancausewidelydistributedacousticlow-velocityzones.Theselow-velocityzonescandeterioratetheseismicsignalandcreateregionsofchaoticseismicsignals.Thenatureandshapeofthischaoticregionofacousticsignalscanvarydependingontheprocessofformationofthesezones.Chaoticregionsinseismicdatacanalsoresultfrommudmobilizationtriggeredbyverticalmigrationof?uids(L?sethetal.,2003).Mudmobilizationcanmodifythestructureofsedi-mentstoadisruptedsuccessionandformalow-densitysediment-?uidmixture.Vertical?uid-?owfeaturesandchaoticseismicre?ectionzonesarecommonlyobservedwithmosttypesofsedi-mentmobilizations(Graue,2000;Hurstetal.,2003;L?sethetal.,2003;JacksonandStoddart,2005).Fluid?owcanalsoalterthe精彩内容，尽在百度攻略：在这个困的睁不开眼得中午，你把我拉了过来，算了，说正题。支持那个游戏，说实话，我支持最开始，国外的我的世界，被网易一代理，作为一名学生党，哪有钱买啊，别说我穷，我真的掏不出来这45块钱，所以说，支持最开始国外的我的世界，迷你没啥可说，把原代码直接搬走了，查的时候还还加密了，明显有见不得人的地方。另外，如果去掉什么抄袭不抄袭，就单看游戏质量，就不一样了，迷你最让人讨厌的应该就是充值系统了吧，家具，玻璃，甚至是床，都要氪金解锁，明显的，很腾讯化啊。想要东西，就要有豆，想要有豆，就要充钱，想要充钱，就得有钱，我哪来的那么多钱玩一个盗版游戏啊，有这钱，买个国服我的世界多好，免费MOD，免费皮肤，免费披防抓取，好心游戏网提供内容，请查看原文。S.Vadakkepuliyambattaetal./MarineandPetroleumGeology43(209楼主没有看过lck，只知道lpl吧。我觉得最强的是s5夏季赛skt，上单marin，打野bengi，中单faker，下路wolf加bang。我是狗粉，首先说为什么ad不选uzi，如果uzi是韩国人，在防抓取，好心游戏网提供内容，请查看原文。formation,causelocalsedimentremobilization,andappearaschaoticre?ectionsintheseismicpro?le(Ligtenberg,2007).Ge-ometryofsubsurface?uid-?owsystemsishardtoconstrainbydirectobservations(Talukder,2012)andcharacterizationofthemisdif?cultbecause?owcanbehighlytransientandcanvaryintimeandspacealongcomplexandchangingconduitsystems(Hornbachetal.,2007).要想逼格高最重要的一点是：走别人没走过的路叔本华曾说过这样一句话：有才之人，能击中别人无法击中的目标；天才，能击中别人连看都看不到的目标。Talenthitsatargetnooneelsecanhit.Geniushitsatargetnooneelsecansee.苹果逼格够高吧？世界首款无键盘全触屏手机IPHONE，谁提出来的？乔帮主乔布斯啊，逼格界的如来佛祖。乔布斯就是这样一个天才，永远能洞察世界的下一步的走向，领先世界五百年看到这你就要说了，现在就连小学生都用苹果手机，烂大街的东西哪还有什么逼格可言OK，你这么说了我也不反对，想要更有逼格的东西请你再看这张图你又要说了，你他妈在逗我？防抓取，好心游戏网提供内容，请查看原文。TheSWBarentsSeaisapartoftheArcticOceanlocatednorthofNorway(Fig.1).Occurrenceofshallowgas,gashydratesandsea-?oorexpulsionfeatureshasbeenreportedfromseveralareasoftheSWBarentsSea(e.g.Andreassenetal.,1990;Perez-Garciaetal.,2009;Chandetal.,;Ostaninetal.,2012).Migrationof?uidsintoshallowsedimentsandseepageintotheoceanthroughthesea?oorwasprobablytheresultofspillageandmigrationofhydrocarbonsinresponsetoupliftanderosionprocessesintheCenozoic(e.g.Doré,1995;DoréandJensen,1996;Henriksenetal.,2011).精彩内容，尽在百度攻略：如果是前期对线的话能打赢他的ADC的确不多，女警，奥巴马和他有的一拼。女警超远射程可以有很好的消耗效果，而且清兵特快，一旦推进了你的塔内，在你方塔下放三角阵或者八字，一字型夹子，那你补兵都不好补，只有呼叫打野。再说说奥巴马，前期超强存在，无论是清兵能力还是前期对拼因为他的被动都非常强，当然拼不过还有E逃跑，对线德莱文真的不好打他。如果要打纯后期单挑，德莱文带Q的斧子甚至可以两刀砍死其他ADC，他也不是完全没ADC是他的对手，如果周围有墙那薇恩一般都可以打赢德莱文R-Q-E-A-A-A-A，但如果出了水银刀的德莱文有点恶心，当然薇恩的三枪真伤也不是闹着玩的，后期很快的攻速可以让她超快的叠满三层被防抓取，好心游戏网提供内容，请查看原文。UpliftanderosionisknowntohaveaffectedtheSWBarentsSeaduringCenozoictimes(Faleideetal.,1996;Dimakisetal.,1998;Anelletal.,2009).Thisprocessisthoughttohaveaverystrongimpactonpetroleumsystems(e.g.DoréandJensen,1996;Bj?rkumetal.,2001;Cavanaghetal.,2006;Ohmetal.,2008;Henriksenetal.,2011).Thenegativeeffectsofupliftandassociatederosiononhy-drocarbonsystemsincludetiltingandopeningofhydrocarbon-?lledtrapsresultinginspillageofoilandgas(KjemperudandFjeldskaar,1992),gasexpansionandex-solutionfromoil(Skagen,1993;DoréandJensen,1996;Cavanaghetal.,2006),sealfailure(e.g.,Sales,1993),reductionintemperatureduetoupliftresultinginimma-turesourcerocks(Doréetal.,2000;Ohmetal.,2008),andporosityandpermeabilityreductionduetodiageneticprocesses(Berglundetal.,1986;Walderhaug,1992).Whereas,positiveeffectsincludetheoccurrenceofthermallymaturedsourcerocksatshallowlevels(Bj?rkumetal.,2001),liberationofdissolvedmethanefromformationwater(DoréandJensen,1996)duetodecreasesinpressure(e.g.Maximovetal.,1984;Nesterovetal.,1990),ex-solutionoflightoilorcondensatefromgas(e.g.PiggottandLines,1991),fractureenhancementoflesspermeablereservoirs(e.g.Aguilera,1995)andremigrationtoshallowerstructures(WaylettandEmbry,1992).Inaddition,localre-depositionunderaheavyoverburdenassociatedwitherosioncanresultinrapidmaturationofsourcerocksandgenerationofhydrocarbons(e.g.DahlandAugustson,1993).首先王者荣耀是属于一个推塔游戏再到团战游戏，而不是各打各的。实事证明车队打排位上分比起单排上分容易2.5倍，车队的胜率也比单排多19%左右。今天聊一下很多玩家都会遇到的情况。如果团灭敌方之后，是集合推高地再推水晶呢？还是打主宰拿九条主宰先锋加强兵线呢？这个时候往往会有队友发出进攻敌方水晶的信号，而有的队友则会发信号打主宰！而此时你如果迟疑几秒，说不定对方英雄就马上复活了。战场上可谓是瞬息万变，犹豫不决的话就会错失良机了！那么到底是推高地，还是拿下主宰呢？先来说说主宰吧，一般情况下，如果队友们都是十一二级的话，打起大龙来会比较吃力。当然了，如果敌方团灭而你们还有五个人，一起打主宰的话，会轻松很多防抓取，好心游戏网提供内容，请查看原文。NumerousglaciationsalsoaffectedtheSWBarentsSearegionduringthelateCenozoic.Rapidbuildupandremovaloficeload,asoccurredintheSWBarentsSea,mayhavelessimpactontheevolutionofthebasin(Lercheetal.,1997).However,distortionstothethermalregimeofsub-icesedimentscausedbyspatialandtemporalvariationsoficethicknessin?uencethegeneration,migrationandpresent-dayaccumulationofhydrocarbons(Lercheetal.,1997;Cavanaghetal.,2006).Iceloadingcancausestruc-turaldistortionsleadingtoaredistributionofgasandoilinthereservoirandspillofhydrocarbons(Lercheetal.,1997).Majorice-loadingeffectsarepresentintheHammerfestBwheremanydrilledwellsfoundonlyasmallamountofresidualoilinrotatedandtiltedstructures(Rasmussenetal.,1993;Nylandetal.,1992).感谢邀请，本人先说明一下，我的世界创始于2009年，迷你创建于啥时候？2015年！说minecraft抄袭垃圾迷你的，咋TM想的你！要你这么说Notch从2009年穿越到2015年抄袭迷你，再跑回去，有病啊！咋不穿越火线呢！那你这么说人家Notch咋不再穿越到2015把垃圾迷你厂家给端了呢？（当然那是不可能的了）所以！看清楚时间！看清楚历史！闲着没事玩什么穿越啊，又不是人家''都''教授（没看过，不知道到底是哪个字）本人再发点图，自己做的。。。这个是搬运的：高兴就好高兴就好，再次，欢迎加入【FMN基金会】大力邀请MC神喷加入，壮大力量！实力爆垃圾迷你！基金会持续时间（2015.12～****防抓取，好心游戏网提供内容，请查看原文。Often,largegasanomaliesoverliehydrocarbondiscoveriesinSWBarentsSeaindicatingleakageofgasfromthedeeperforma-tions(Chandetal.,12;Heggland,;Meldahletal.,2001).ArecentstudyfromtheLoppaHigh(Chandetal.,2012)reportedseepageofgasintothewatercolumnindi-catingthatthegasmigrationisstillactivethroughopenfaults.Thelocationsoftheseanomaliesmayindicatepossibletargets精彩内容，尽在百度攻略：说《诛仙》与《七界传说》齐名，估计你会被喷出个爆款??我是看过的，这本书一开始还是不错的，后来吗，个人感觉有几个问题，1.各界的塑造不够，人物略少，整体缺乏“界”的气势，直观感觉其实都和一个门派差不多。2.人物刻画不足，女人们基本都是男主的迷妹，男人们有特色的没记住什么，男主令人印象最深刻的是他的种马，竟然连他一个师傅都难逃魔迪奥，在武侠仙侠这种尊师重道的小说中，这种情节太过违和，传出去绝对被各路小说中的世人所不齿，所以小说中也无人知晓。3.男主其实不是什么草根平民，而是天赋异禀的绝世高手后代，并且配备绝世神器，含着钻石钥匙出生，和主流的草根主角比略有逊色，毕竟看网文的大部分人还是更接近草根（防抓取，好心游戏网提供内容，请查看原文。forFigure1.GeneralbathymetricmapofSWBarentsSeawithmajorbasinsandhydrocarbondiscoveries.Thelocationofthestudyarea(redstar)andseismiclinesinthefollowing?guresarealsoshown.精彩内容，尽在百度攻略：谢邀。首先说一下王者荣耀的评分系统，根据你的击杀数，被杀数，助攻数还有参团率等一系列因素给你的评分。首先这个分数在有些情况下是很不合理的。举个栗子，李元芳打野很强，抢大龙小龙很快，偷到主宰对团队的贡献很大吧，但是在最后评分无法体现。通常两边正常打不送不放水的情况下两波主宰会推掉对面两三座塔甚至更多，但是这在评分上没有体现。所以分数只是一个参考，高分并不代表厉害，低分也并不代表很坑，我用猴子在劣势的防抓取，好心游戏网提供内容，请查看原文。210S.Vadakkepuliyambattaetal./MarineandPetroleumGeology43(谢谢小秘书邀请(????)王者荣耀玩猴子用什么名字？个人认为玩猴子不一定非要去用与猴子相关的名字，既然题主就是有这样的需要，我绞尽脑汁想到了几个我个人认为还不错的名字。吃我一棒放屁都暴击齐天如果感觉只防抓取，好心游戏网提供内容，请查看原文。futurehydrocarbonexploration.Therefore,itisimportanttoun-derstandthedistributionof?uid-?owanomaliesandtheirgov-erningcontrols.Here,weanalyze2DseismicdatacoveringthewholeSWBarentsSea(Fig.2)inordertodelineateandclassifyvarious?uid-?owfeatures,tocharacterizetheirdistribution,andtobetterunderstandtheirrelationtothestructuralsetting,glacia-tions,uplift,anderosionduringtheCenozoic.2.Geologicalsetting首先得看你在哪里，比如:1你在亚洲中国等地那你最先思考的是应该躲在哪里，毕竟这里禁枪人口又太密集，好一点的刀具也没多少，况且咱们又不是啥主角什么的出门就能捡个三棱军刺的，但是菜刀之流的千万别要拿，那玩意砍人太钝又太短，所以长棍是不错的，如果有信心可以去派出所和城管局刷装备，枪啊防爆盾什么的都是有的，但是体力不好的话就穿一套防刺服就行了，长电棍可以找一找的没有也没关系警棍可以前期勉强凑合一下。2你在美国的话趁爆发没多久赶紧跑路，随便抢一辆车，记住警车里面都是有手枪的（枪店就别想了那太大众话了轮不到你的），不要去飞机场那些大众化的逃生地点去郊区，山区或者海边躲起来，老美的环境保护还是可以的你可以自防抓取，好心游戏网提供内容，请查看原文。2.1.Geologicalhistoryofthearea精彩内容，尽在百度攻略：战局逆风不放弃逆风翻盘是一件多么痛快的事情，有过经验的玩家都应该了解，战局逆风不代表输赢，万一对面浪了呢？万一对面吵架了呢？万一对面五个人打团就460呢？万一对面五个人掉线了呢？王者荣耀即将来到了赛季防抓取，好心游戏网提供内容，请查看原文。TheBarentsSeaisalargeepi-continentalsea,boundtothewestandnorthbyyoungpassivemarginsthatdevelopedduringtheCenozoicopeningoftheNorwegianeGreenlandSeaandEurasiabasin,respectively(Faleideetal.,1993).TheSWBarentsSeacon-tainssomeofthedeepestsedimentarybasinsworldwidewithsedimentcoverexceeding10kmatplaces(e.g.NordkappBasin,S?rvestsnagetBasin)(Smelroretal.,2009).ThesebasinsformedinresponsetoseveralphasesofregionaltectonismwithintheNorthAtlanticeArcticregion,culminatingwithcontinentalseparationofEurasiaandGreenland,andaccretionofoceaniccrust,intheearlyTertiary(Faleideetal.,1993).怎么说，第一次有想写长篇评论的冲动……也许是刚刚看完b站楚河的录播的缘故吧……昨天看楚河直播，说是双方水军一个劲的带节奏，能看出来，是想给自己和对方一个台阶下，不想事情越搞越大，伤害的都是双方。没成想今天就彻底撕破了脸……王者荣耀我是个看张大仙直播的，对于嗨氏，只能说是路人吧，但还是偏好感，在头条上能看到他的短视频，感觉是和大仙一样的好少年。但是，看完今天楚河长达90分钟的录播……我觉得我是瞎了眼的。不去管嗨氏与董导恩怨，与猴三棍恩怨，与小潮恩怨，与楚河恩怨……甚至楚河说的什么要跳槽斗鱼，因为尽管他放出来很多视频，但是不了解不评论……但自行了解了一下画手事件然后是真的愤怒了什么是画手？嗨氏的这防抓取，好心游戏网提供内容，请查看原文。ThewesternpartoftheBarentsSeashowsmuchmorecomplextectonicdevelopmentthantheeasternpart,withamosaicofba-sins,platforms,andstructuralhighs(Faleideetal.,1984;Gabrielsenetal.,1990;Gudlaugssonetal.,1998).TheSWBarentsshelfformedacentralpartofthenorthernPangeanmarginfromthelateDevonian(Worsley,2008)andisunderlainbyearlyDevonianmetamorphicbasementformedduringtheCaledonianOrogeny(Smelroretal.,2009).ExtensionaltectonicmovementsduringearlyemiddleDevonian,Carboniferous,Permian,TriassicandlateJurassiceearlyCretaceous(Johansenetal.,1993)dominatethelatePaleozoicandMesozoictectonichistoryoftheSWBarentsSea.ExtensionalfaultingalsoaffectedtheregionduringlateCretaceousandPaleogene(Faleideetal.,1993).InlateDevoniantoearlyCarboniferoustimes,mostoftheBarentsSeawasaffectedbycrustalextension(Gjelberg,;Faleideetal.,1993).TheseriftingeventscausedtheformationofHammerfestBasinasaNE-trendinghalfgraben(Cavanaghetal.,2006).EvaporitesweredepositedintheNordkappBasinandpossiblyalsointheTroms?Basin(Worsley,2008).ExtensionalfaultingaffectedtheLoppaandtheStappenHighsduringlateCarboniferoustoearlyPermianperiod(BrekkeandRiis,1987),whilenortheasternpartofBjarmelandPlatformandNordkappBasinwerestable(Riisetal.,1986).大司马――我的梦想是开一家真皮网咖，本名韩金龙，是斗鱼直播平台旗下的一名签约主播。主播的内容当然是英雄联盟。直播时间段固定在每天下午三点到晚上八点，周三固定休息。其他时间段没特殊情况一般都会播。你是李时珍的皮，一生之敌愣头青！非常喜欢马老师的直播，幽默。马老师的贴吧微博都可以关注一波，时不时会有些小福利哟~~防抓取，好心游戏网提供内容，请查看原文。ThewesternpartoftheBarentsSeahasbeenthemosttecton-icallyactivesectorthroughoutMesozoicandCalthoughTriassictoearlyJurassicwasrelativelyquiettectonically(Gabrielsenetal.,1990).However,reactivatedriftinginthePermian-earlyTriassicledtotiltingintheLoppaHighandStappenhighregion(Fig.1)(Gudlaugssonetal.,1998).TheearlyTriassicwascharacterizedbyregionalsubsidenceineasternareasandsedimentin?uxintotheregionalsagbasinfromtheEast(Gudlaugssonetal.,1998;Worsley,2008).Salttectonicsin?uencedthedepositionalpatternsintheNordkappandMaudBasins(Fig.1)(Gabrielsenetal.,1990).精彩内容，尽在百度攻略：怎么样才可以一次抽到王者水晶呢？小编觉得很简单啊，想要一次就抽到王者水晶，最重要的就是要看你的RP好不好了。在王者荣耀中，王者水晶现阶段只能通过幸运夺宝来获取。王者荣耀王者水晶确实不是那么好抽，说到抽奖，玩家的运气是很重要的一部分，幸运的玩家一下就抽到了也不是不可能，小编就看到贴吧有人33的幸运值就抽到了，所以想要抽的玩家都要相信自己的运气，如果你连自己都不相信，那么幸运女神都不会帮助你了，幸运值的上限是250，每次抽奖幸运值都会上涨，幸运值越高的玩家，抽到王者水晶的概率就越高，已经拥有韩信的玩家也可以通过王者水晶来兑换韩信的皮肤教廷特使，现在还有一个兑换的物品还没有列出来，有可能是其他英雄，防抓取，好心游戏网提供内容，请查看原文。Riftingandassociatedblock(extensional)faultingstartedagainintheMid-Jurassic,relatedtotheopeningofCentralAtlantic(Ziegler,1988),increasedduringtheperiodfromlateJurassicintoearlyCretaceous,withtheopeningofsouthernNorthAtlantic(Faleideetal.,1993),andterminatingwiththeformationofthenowwell-knownmajorbasinsandhighs(Fig.1).今天是全中国和全高考生的大日子，那就是高考。对于高考想必很多人都是紧张的，尤其是家长和考生，三年来的努力都在7、8、9三日里体现了，在此小编也祝各位能够取得一个好成绩，上自己理想的大学。对于考试紧张压力大想必是...今天是全中国和全高考生的大日子，那就是高考。对于高考想必很多人都是紧张的，尤其是家长和考生，三年来的努力都在7、8、9三日里体现了，在此小编也祝各位能够取得一个好成绩，上自己理想的大学。对于考试紧张压力大想必是很多考生必不可免的，但是玩游戏玩太久，导致错过了高考的话，那就真是尴尬了！今天就有一个小伙伴，由于高考紧张压力太大，昨晚玩了三个小时的王者荣耀，结果早上睡觉睡过头了，导致自己防抓取，好心游戏网提供内容，请查看原文。Structural精彩内容，尽在百度攻略：致Minecraft有一种游戏，叫做Minecraft.....我忘不了第一次玩MC的时候，撸掉的第一块原木，挖到了第一块钻石，第一次被苦力怕炸死，第一次见到末影人，并且怀着好奇心去和他对视，第一次找防抓取，好心游戏网提供内容，请查看原文。Figure2.Coverageof2Dseismicdata(thinblacklines)usedforthestudywithmajorbasinsandboundaries(thickblacklines)inthearea.应该是我的世界好玩，添加一些mod，光影材质，动态光影，add-ons，皮肤，披风之类的。迷你世界的mod，皮肤，披风，add-ons，光影材质，动态光影都没有，而且这些有些要钱，里面的物品还要等级解锁，真服了这些迷你玩家是怎么玩下去的，联机方便怎么了，即使我没有盒子，我的世界也有自带的联机，只需输入电脑上的ip地址就行，在创建个世界，开启局域网世界。虽然是国版，但是也不能这么抄袭别人吧，那些支持防抓取，好心游戏网提供内容，请查看原文。S.Vadakkepuliyambattaetal./MarineandPetroleumGeology43(211一如果是在游戏里打架的话那肯定MC赢咯，MC就是不用MOD不用指令不开创造，仗着人多也能把迷你狗们打到喊爹吧，适合打架的MOD我看非无尽贪婪莫属，无尽套穿满后不会再受到任何伤害，剑的伤害是∞，也就是说防抓取，好心游戏网提供内容，请查看原文。developmentinthisperiodwascomplicated.Ononehand,extremeratesofsubsidenceareseenintheTroms?BasinandthewesternpartoftheBj?rn?yaBasinduringtheearlyCretaceous(AptiantoAlbian).Ontheotherhand,indicationsoflocalearlyCretaceousinversionarefound,e.g.alongtheRingvass?y-LoppaFaultComplex(RLFC)anditsjunctionwiththeAsteriasFaultComplex(Fig.1)(Gabrielsenetal.,1990).DuringtheearlyCreta-ceous,Harstad,Troms?,andBj?rn?yabasinsunderwentlarge-scalesubsidenceandbecomemajordepocenters(Faleideetal.,1993).UpliftanderosioninthenortheasternBarentsSeabroughtmoresedimentsintothesedepocenters(Smelroretal.,2009).ThroughouttheCretaceous,riftingprevailedandcausedformationofpull-apartbasinssuchasS?rvestsnagetBasinandVestbakkenVolcanicProvince(Fig.1)(Smelroretal.,2009).Inthewesternpartofthearea,especiallyintheVestbakkenVolcanicProvince,therewasabundantmagmaticactivity,probablyinthePaleoceneandEocene(JebsenandFaleide,1998;Faleideetal.,2008).精彩内容，尽在百度攻略：必须英雄联盟难啊！不要把手游的难度和端游来做比较，没有任何可别性的！那些扯什么王者荣耀难的，别逗我笑了，本人长期混迹于LOL一区白银，打王者荣耀目前没有一个赛季不在钻石以上。别说什么王者荣耀用户基数大，难度大。正是因为基数太大，所以坑才多，水平层次不齐。会玩的不会玩的都能混迹于各个分段，所以这个游戏上分才容易。你去和DOTA2比一比，那个游戏人少，但现在能坚持玩的都是老玩家，你现在作为新手进去，看看你能上分不？估计低分段都能虐的你怀疑人生，所以别说什么人多上分就难，都是扯淡。还有相对于王者荣耀，英雄联盟需要更多的配合，里面的不合理现象很少很少，平衡性更好，需要技术，意识，团队合作更高一点，王者防抓取，好心游戏网提供内容，请查看原文。TheopeningoftheNorthAtlanticwasassociatedwithupliftduringthePaleocene-Eocene(Eldholmetal.,1987;Faleideetal.,1996).InversionandfoldingreachedamaximuminEocenetoOligocenetimes(TalwaniandEldholm,1977;Myhreetal.,1982;Eldholmetal.,1987).自救守则：生化危机爆发应对手则，同样适用于战争（战争比生化危机还恐怖，面对的飞机大炮笔者宁愿面对丧尸）假设在生化潮爆发前一个月只有你一个人知道，社会稳定，市场秩序井然，那么首先恭喜你，你有一个很好的开头，那么我们在这样一个完美开头的情况下，我们开始做我们的灾后准备：1.首先我们有50万，那么我们第一要做的就是找更多的钱来换取物资，什么网贷越快越好，再换10万，反正不用还，这样起始资金有了60万.2.统计你要救的人，以我自己算，我、我父母、妻子、孩子（记住在末世的情况下，人性是险恶的，不要乱发善心，会害死你，带上能为你付出生命的人，其他人就算了）5个人.3.交通工具和生存工具：租辆大货车（不要买防抓取，好心游戏网提供内容，请查看原文。TheBarentsSeawasaffectedbyextensiveerosion,relatedtodeglaciationandupliftinthelatePlioceneePleistocene(Vorrenetal.,1991;Nylandetal.,1992).DuringlatePlioceneePleistocene,theentireBarentsShelfwasupliftedanderoded,andlargeamountsofsedimentweredepositedalongthewesternmargin(Nylandetal.,1992).ParticularlylargeaccumulationsarefoundintheBj?rn?yatroughmouthfan(Fig.1),withupto6km-thickpackagesofglacigenicsediments,amaindepocenterduringthelateCenozoic(Hjelstuenetal.,2004;Vorrenetal.,1991).InthesouthernpartoftheSWBarentsSea,theHammerfestBasin,theNordkappBasinandtheLoppaHighsufferedlesseramountsofupliftanderosion(Smelroretal.,2009).TheUpperRegionalUn-conformity(URU),formedduringthelatePlioceneePleistoceneatabout2.5Ma,separatestheglacigenicsedimentsoftheBarentsSeafromthedeeperpre-glacialsedimentaryrocks(Tertiaryandolder)andisamajorseismicre?ectorinthestudyarea(SolheimandKristoffersen,1984;Eidvinetal.,1993).Criss-crossingglacialline-ationsandicebergploughmarksareamajorfeatureoftheBarentsSeaseabedandpaleoseabedsaffectedbyglacialerosion(Elverh?iandSolheim,1983;Andreassenetal.,2007b).2.2.Majorsourceandreservoirrocks丧尸危机末日即将来临，人类文明一夜消失。没有救援，没有希望，我们各国幸存的老百姓及军队能否在满是丧尸的世界中与自己的爱人重逢和战斗？幸存下来的各国老百姓，是否能战胜这场看似无穷无尽的灾难，重建自己的家园？属于人类的亲情、友情、爱情，一切人性中美好的事物将会在这里升华；背叛、贪婪、自私，人性中的丑恶永远也不会与美好分离。注：本文部分内容源自马克思?布鲁克斯（MaxBrooks）的《丧尸生存手册》，和网络上流行的《末日求生指南》。危机爆发前如果能够遇见生化危机爆发，作为手上只有10元的中国普通老百姓。你的资源过于贫乏，甚至无法通过一些正常的购买手段来囤积生存物资。如果你是官员或者富豪，那么你的求生防抓取，好心游戏网提供内容，请查看原文。Numeroussource-rockformationsarepresentintheSWBarentsSea(Fig.3)(Doré,1995).Theamountoftotalorganiccarbon(TOC),hydrocarbongenerativepotential,andhydrogenindexofvarioussourcerocksintheNorwegianBarentsSeaarediscussedindetailbyOhmetal.(2008).Themostwidelydistributedandmostproli?csourcerockistheHekkingenFormationoflateJurassicage,whichconsistsofdark,organicrichshales(Dallandetal.,1988).DespitebeingwidespreadovermostofthesouthernBarentsSea,theseshaleshavenotrealizedtheirfullhydrocarbon-generationpotentialbecauseofvaryingdepthofburialandtherebymaturity.TheunitisthoughttobematureforoilandgasgenerationinanarrowbeltatthewesternmarginoftheHammerfestBasinandalongthewesternfringeoftheLoppaHigh(Doré,1995).HekkingenshalealsohasthehighestTOC,highesthydrocarbongenerativepotential,andhydrogenindexamongthesourcerocksintheNorwegianBarentsSea(Ohmetal.,2008).精彩内容，尽在百度攻略：首先，其他人的回答都没抓到点子上。我手上就有一台小米5s，我来告诉你为什么这么卡！其实这是因为小米的温控降频锁核阻碍了你愉快地玩王者荣耀，目前解决的办法主要有两点∶一、想办法把手机电池的温度降到40摄氏度以下(温控是按电池温度来控制CPU的)。可以选择吹空调风扇之类的，不大推荐放冰箱，手机容易受潮(我将纸巾叠成方块然后沾水贴在手机背部再对着风扇玩，湿巾纸买不起，吹空调冷手受不了)；二、root之后用“温控拜拜”。让你的阉割版火龙821满血复活！同时配合“高通骁龙CPU锁核心方案”，获得更持久的游戏体验！但是还是要注意降温，复活的火龙发热极为严重，别把手机烧坏了。。。顺便说一下，之前问了一下RO防抓取，好心游戏网提供内容，请查看原文。Triassicshalessuchas,SnaddFormationandHavertFormation,arealsoshowntohavepotentialforgeneratinghydrocarbons(Bjor?yetal.,2009).Thecumulativegenerationpotentialfromthe1.饥荒饥荒主人公威尔逊是个实验失败的科学家，一次实验时打开了收音机，收音机却传给他禁忌的知识，他造出了时空穿越器，启动后却不小心被传到了饥荒的时代。每个地图都会随机生成一个麦斯威尔的传送门，通过十五关有小弥弥，这看似是个勇士打败恶龙却变成恶龙的故事，实际背后的故事很有意思，不过我是个新手活不过第一晚∏_∏2.贪吃蛇大作战这个游戏是操纵一条小小蛇杀死其他蛇变大大粗粗蛇的游戏，据说国外有个大神玩到了防抓取，好心游戏网提供内容，请查看原文。thickTriassic(andpossiblyLowerJurassic)sedimentarypileislarge,anditiswidelyassumedthatthemajorgasdiscoveriesoftheSouthBarentsBasinemanatefromthissource(Johansenetal.,1993).PermianandCarboniferousshalesarethemajorsourceofhydrocarbonsintheFinnmarkPlatform(Ohmetal.,2008).当然是选贵的....如果是只送一个的话……荣耀水晶与王者水晶兑换的最好。芈月：大秦宣太后（用了红桃皇后代替一下....）小乔：天鹅之梦钟无艳：海滩丽影孙尚香：杀手不太冷（没找到图.....）韩信：教廷特使（首先你要有韩信）再下面就是贵哒了荆轲：暗夜猫娘鲁班：电玩小子墨子：龙骑士项羽：苍穹之光不过谁会送你皮肤呢……防抓取，好心游戏网提供内容，请查看原文。Figure3providesasummarybygeologicalageofallmajorsourcerocksandreservoirs,provenandpostulated,intheNor-wegianBarentsSea.Themostsigni?cantproportionofthehydro-carbonresourcesproventodateinboththeNorwegianandRussianBarentsSeaaretrappedwithinstrataofJurassicage(Doré,1995).ThemajordiscoveriesintheSWBarentsSeahaveprincipalreser-voirsconsistingofloweremiddleJurassicsandstonecalledtheSt?Formation(Dallandetal.,1988).Larsenetal.(1993)estimatethatabout85%oftheNorwegianBarentsSearesourceslaywithinthisformation.MinorTriassicgasaccumulationshavebeenfoundintheHammerfestBasinandonthemarginsoftheNordkappBasin.3.Dataused精彩内容，尽在百度攻略：The?uid-?owfeaturesweremappedusingapproximately30002Dmulti-channelseismicpro?lescoveringtheSWBarentsSea(Fig.2).Inadditiontotheseismicdata,welllogswithformationtopsfrom60wellsintheSWBarentsSeaaidedtheinterpretation.The2Dlineswerefromdifferentsurveyswithdifferenthorizontalandverticalresolutions.4.Observationandinterpretationof?uid-?owanomaliesMulti-channelseismicdatafromdifferentbasinsoftheSWBarentsSeaareusedformappingvarioustypesof?uid-leakageanomalies.Mappingofthesourceof?uid-?owanomalieswasoftendif?cultbecauseofvaryingsurveyspeci?cationsinresolutionandseismic-signalquality.The?uid-?owfeaturesinterpretedonseismicdataweresubdividedint1)?uid/2)leakagealongfaults,and3)allotherfeatures,notincludedinthe?rsttwocategories.4.1.Fluid/gaschimneysManyoftheseismicpro?lesfromthestudyareashowzonesofchaoticacousticsignalsand/oracousticmasking(Fig.4).Thesizeandshapeoftheseacousticallyanomalouszonesvarieswidely.Inmostparts,theseanomalouszonesterminatedatdifferentshallowstratigraphiclevelsshowinghigh-amplitudeanomalies,suggestingthepresenceofgas.Suchfeaturesareinterpretedasgaschimneys,whichcanbede?nedasaregionofdistortedseismicsignalsresultingfromirregularlydistributedlow-velocitygas-chargedzones,formedduetoanupwardmigrationofgas/?uids(Meldahletal.,2001;L?sethetal.,2002;Heggland,2004;JuddandHovland,2007;Arntsenetal.,2007;Connollyetal.,2008).Figure4(a)showsgaschimneyslocatedintheBj?rn?yaBasinwestoftheLoppaHigh.Theyshowwell-de?nedzonesofchaoticseismicsignalsandterminateattheTopCretaceouslevel.Patchyhigh-amplitudere?ectionswereobservedabovebothchimneys.Thesmalldepressionsonthesea?oorwereinconclu-siveforpockmarks,sincetheareawasglaciatedinthepastandthusthedepressionsmaybeglacialploughmarks.ThegaschimneysarelocatedintheBj?rn?yrennaFaultComplex(BFC)area(Fig.1),andthesmallgaschimneyislocatedrightaboveafault(Fig.4a).Wehypothesizethatthegasmigratesupwardthroughthisfault.SeismicdatafromthePolheimSub-platformwestoftheLoppaHighshowsanexceptionallylargegaschimney(Fig.4b).Averylargezone,approximately12kmwide,ofacousticmaskingcharacterizesit.Shallowhigh-amplitudere?ectionsmarktheupperterminationofthechimney.High-amplitudeanomalies精彩内容，尽在百度攻略：212S.Vadakkepuliyambattaetal./MarineandPetroleumGeology43(Figure3.SomemajorprovenandpotentialreservoirandsourcerocksintheBarentsSea(modi?edafterDoré,1995;Ohmetal.,2008).arepatchy,polarity-reversedandcrosscutsomepartsofthelithology.Theseismicsignalishighlychaoticinsidethechimney,makingitdif?culttoidentifythesourceofgasleakage.However,theareaispartoftheBFCandthe?uidmigrationcouldbealongthesefaults.精彩内容，尽在百度攻略：Verticalandlateralmigrationof?uidsisvisibleinS?rvestsnagetBasinclosetoVeslem?yHigh(Fig.4c).High-amplitudeanomalieslocatedatthePlio-Pleistoceneboundary(URU)marktheupperterminationofacolumnarzoneof?uidmigration.Thehigh-amplitudereversepolarityre?ectionsatthisstratigraphiclevelsuggestaccumulationofgas.Thisfeatureisinterpretedasagaschimney.High-amplitudere?ectionsarealsovisibleonotherstratigraphicboundariesadjacenttothegaschimneyandawayfromtheterminationpointofthechimney,suggestinglateralmigrationintheup-dipdirectionalongthestrata.TheseismiclinelocatedonthesoutheastpartofLoppaHigh,closetothejunctionofAsteriasFCandRLFC(Fig.1),showsanotherexampleofagaschimney(Fig.4d).Theregionof?uidmigrationismarkedbyazone,approximately1-kmwide,ofseismicre?ectorsthatarechaoticanddeterioratedinamplitude.Faultsmay精彩内容，尽在百度攻略：beS.Vadakkepuliyambattaetal./MarineandPetroleumGeology43(213Figure4.a)Show?uid?owinthesoutheastpartofBj?rn?yaBasin.Theleakagezoneoflarge?uid?owfeatureisw8kmatitswidestregion.Patchyhigh-amplitudeanomaliesarepresentontopoftheleakagezone.Theleakagezonecoversanareaofw36km2.Thesmallchimneysitsontopofafaultandshowsbrightspotsontopofthetermination.b)A12kmwide?uidmigrationfeatureSWoftheLoppaHigh.Itcoversanareaofw130km2.Theshallowhighamplitudere?ectionsshowreversepolaritywithrespecttothesea?oorindicatingpresenceofgas.Theyalsocrosscutslithologicalre?ectorssuggestingformationofgashydrates.c)Seismicpro?lefromS?rvestsnagetBasinclosetoVeslem?yHighshowschaoticacousticsignals,whichterminatesinLateTertiarysedimentsleavingbrightspots.Thisfeatureisinterpretedasagaschimney,andthehigh-amplitudeanomaliesindicatethepresenceofgas.d)ShowsagaschimneyfromtheSWpartofLoppaHigh.Highlychaoticseismicre?ectorsde?nethezoneof?uid?ow,andaverybrightre?ectorisvisibleontheterminationpointofthechimney,suggestingaccumulationofgas.精彩内容，尽在百度攻略：presentinsidethechimney,butaredif?culttoidentifyintheseismicpro?leduetolossofseismicenergyinsidethechimneyzone.Averystrong,polarityreversedre?ectorattheterminatingpointofthechimneyjustbeneaththeURUre?ectorsuggestsaccumulationofgas.TheSnaddFormation,oneofthemajorsourcerocksinthearea(Fig.3,Section2.2)andotherdeepersourcerockscouldbethesourceof?however,itisverydif?culttoidentifyitaccuratelyfromtheseismicdata.精彩内容，尽在百度攻略：214S.Vadakkepuliyambattaetal./MarineandPetroleumGeology43(4.2.Leakagealongfaults2Dseismicdatashowchaoticre?ectionsandhigh-amplitudeanomaliesassociatedwithfaultsinmanypartsoftheSWBarentsSea(Fig.5).Aseismicpro?lefromthenorthernpartoftheLoppaHighshowstwomajorfaults,cuttingthroughtheHekkingenFor-mationandextendinguptotheURU,associatedwithseveralminorfaults(Fig.5a).Highlychaoticandlow-amplitudere?ectionsoccurclosetotherootofthemajorfaults,suggesting?uidmigrationfromamuchdeepersourceandbranchingof?uidmigrationalong精彩内容，尽在百度攻略：theFigure5.a)Seismicpro?lefromnorthernpartoftheLoppaHighshowsleakagealongfaultsintheHekkingenformation.Thetwomajorfaultsactasmainpathwaysforleakage.Accompanyingminorfaultsalsoshowssignsof?uid?owwithhighamplitudeanomaliesontheir?anks.The?uid?owfeatureisnarrowatthebase(w2km)andspreadsasitgoesupcoveringanareaofw290km2.b)Shows?uidleakagealongfaultsfromthesouthernpartoftheLoppaHigh.ThesourceoftheleakagecouldbeearlyTriassicHavertFormationortheunderlyingPaleozoicstrata.c)FluidleakagealongfaultsfromthenorthwestpartoftheHammerfestBasin.Twofaults,oneofthemcuttingthroughtheJurassicHekkingenformation,showhigh-amplitudeanomaliesalongthemandattheirterminationintheshallowstrata,indicatinggasmigrationandaccumulation.Hekkingenformationcouldbethesourceoftheupwardmigratinggas.d)Seismicpro?leacrosstheSamsonDome,NEoftheHammerfestBasin,showw7kmwideregionof?uidmigrationalongfaults.Theleakagezoneisonthesouthernpartofthedome,coveringanareaofw141km2.精彩内容，尽在百度攻略：S.Vadakkepuliyambattaetal./MarineandPetroleumGeology43(215faults.High-amplitudeanomaliesarevisiblealongthefaultplanesclosetotheterminationofthefaults.Occurrencesofhigh-amplitudeanomaliesinseismicdataalongthefaultsindicatethatgasispresent(L?sethetal.,2009;Cartwrightetal.,2007;Ligtenberg,2005).Minorfaultsalsoshowhigh-amplitudere-?ectionsalongfaultplanes.Nohigh-amplitudere?ectionsareobservedabovetheURU,suggestingtrappingofupwardmigratinggasatorbeneathURU.Hekkingenformationcouldbethesourceofshallowgasinthisarea,althoughdeeperformationscouldalsocontributetothegasleakage(SeeSection2.2).Figure5(b)showsaheavilyfaultedregionfromthesouthernpartoftheLoppaHigh.Noisyseismicre?ectionsarevisibleclosetoandalongthefaults.Italsoshowshigh-amplitudere?ectionsonthefaultplanesclosetotheterminationpointoffaults,suggestingpresenceofgas.Afewfaultsextendalmostallthewaytothesea?oorandtheirterminationcoincideswiththeoccurrenceofsmalldepressionsonthesea?oor.Basedonthe2Dseismicdatawecannotresolvewhetherthesedepressionsarepockmarksornot.The?uidmigrationisalongtwomajorfaultsinthedeeperpart,andbranchesoutthroughmanysmallerfaultsintheshallowstrata.TopHavertformationofearlyTriassicagecouldbethemajorsourceofhydrocarbons.Deeperformationscouldalsobecontributingtotheleakage(SeeSection2.2).Seismicpro?lefromnorthwesternpartoftheHammerfestBasinshowsaperfectexampleof?uidleakagealongafault(Fig.5c).High-amplitudere?ectionsoccuralongthestratigraphichorizonsoverclosedistancesawayfromthefaults.The?uidleakageismainlyalongthebiggerfaultuntilTopCreta-ceouslevelandthenbranchesalonganotherfault.High-amplitudere?ectionsarevisibleclosetotheterminatingpointofthefaults,suggestingshallowgasaccumulation.ThemainfaultcutsacrosstheTopofHekkingenformation,whichcouldbethesourceofleakinggas(Doré,1995).TheSamsonDomeareaintheBjarmelandPlatform,northeastoftheHammerfestBasin(Fig.1),shows?uidleakageandshallowgasaccumulationoverananticlinalstructure(Fig.5d).Noisyzonesofseismicsignalsandhigh-amplitudeanomaliesclosetothesea?oorsuggestupwardmigrationof?uids.ThetopoftheanticlinalstructuremarkedbythelateJurassicHekkingenFormationandformationsbelowshowmanysmallfaults,formedprobablyduetoextensionalforces.Thesefaultsmaybeactingasmigrationpathwayforhydrocarbons.Muchlargerfaultsarealsopresentonthe?anksoftheanticlinalstructureandmayalsoplayarolein?uidmigration.TheHekkingenformationisaunitwithhydrocarbonpotential,butisnotmatureinthisarea(Doré,1995).MuchdeeperTriassicformations,suchasHavertfor-mation,couldbethesourceofupwardmigratinggas(Fig.3).4.3.Otherfeatures精彩内容，尽在百度攻略：Manyseismicexpressionsassociatedwith?uid?owotherthangaschimneysandleakagesalongfaultsarepresentintheSWBarentsSea.Thesefeaturesincludeseepagepipes,pockmark-likedepressions,acousticpulldownsrelatedto?uidmigration,andbottom-simulatingre?ectors(BSR).Theyarerareandwidelydistributedinthestudyarea.Seepagepipesarecolumnarzonesofdisruptedre?ectionswithlocalizedamplitudeanomalies(Cartwrightetal.,2007).Pockmarksaredepressionsontheseabedresultingfromtheseepageofgasandpore?uidsinsoftsediments(JuddandHovland,2007).Pockmarksofdifferentsizesandden-sitiesarecommoninsomepartsoftheBarentsSea(SolheimandElverh?i,1985;HovlandandJudd,1988).ThecentralBarentsSeashowsseabeddepressionsupto1000mindiameter(SolheimandElverh?i,1993;Lammersetal.,1995).BSRsarehigh-amplitudereverse-polarityre?ectionsresultingfromabruptchangeinacousticimpedanceattheboundarybetweenahydrate-bearinglayerandunderlyinggassysediments(SloanandKoh,2007;JuddandHovland,2007).Figure6(a)showsavertical,narrowzoneofacousticdisturbancefromthesouthernpartoftheBjarmelandPlatformnorthofNorselHigh.Thezoneofchaoticseismicsignalsterminatesinshallowstrata.However,faults(oneofwhichextendstothesea?oor)arevisibleabovetheterminationpointandthesefaultsmayrepresentpathwaysfor?uidmigrationupwardsthroughthestrata.High-amplitudere?ectionsarevisibleabovethetermi-nationoftheverticalzoneof?uidleakage.Thezoneisapproxi-mately800-mwideandsuchregionsofnarrow,vertical?uidmigration,andisinterpretedasaseepagepipe.Thesourceof?uidleakagecouldbeTriassicorolderformations,sincetheleakagezonegodeeperthantheHavertformationrepresentingearlyTriassic.Aseismicpro?lefromcentralpartoftheFinnmarkPlat-formshowschaoticzonesofseismicre?ectorsandhigh-amplitudeanomaliesindicatingmigrationof?uids(Fig.6b).There?ectorsshowacousticpulldownsuggestingpresenceoflow-velocityma-terial,possiblygas.Thesourceof?uid?owcouldbeearlyPermian/lateCarboniferous?rnformationormuchdeeperCarboniferousshales(Fig.3,Ohmetal.,2008).Alsovisibleisacrater-likedepression,1.2kmwide,whichcanbeinterpretedasapaleochannel.TheBj?rn?yrennaFaultComplex,westoftheLoppaHigh,showsagaschimney,6km-wide,withhigh-amplitudere?ectionsatitsshallowterminatingpoint(Fig.6c).Thechaoticregionintheseismicdatasuggestsupwardmigrationof?uids.High-amplitudere?ectionsobservedabovethechimneyarepolarityreversedwithrespecttothesea?oor,suggestingaccumulationofgasbeneathit.Theseenhancedre?ectionsarealsodiscontinuousandcrosscutstratigraphicboundariesnearit.Thiscrosscuttingeventcanbeinterpretedasagas-hydrate-relatedBSR(Holbrooketal.,1996;Kvenvolden,1998).Higher-orderhydrocarbongasescouldbemigratingalongwithother?uidsthroughthechimneyandcanformgashydratesinthispartoftheBarentsSea(Chandetal.,2008).BSRshavebeenobservedinseismicdataearlierinthisareaandaresuggestedtohavegascompositionwithfewpercentsofethaneandpropanealongwithmethane(LabergandAndreassen,1996).精彩内容，尽在百度攻略：Althoughnohigh-resolution3D-seismicmultibeamdatawereusedforthisstudy,wewereabletoidentifypossiblepockmark-likedepressionsinsomeareas.ItshouldbekeptinmindthattheSWBarentsSeawasheavilyglaciatedintheCenozoicandglacialploughmarksareverycommoninthestudyarea.Thismakesidenti?cationofsurface?uid-expulsionfeaturesdif?cultwith2Ddata.However,seismicpro?lesfromtheBj?rn?yafanshowedpockmark-likedepressionsonthesea?oor,approx.600mwide(Fig.6d).Thesedepressionsshowedverticallystackedhigh-amplitudere?ectionsunderneaththem.Re?ectorsunderneaththechannelshowedacousticpulldown.Thehigh-amplitudere-?ectionssuggestthepresenceofgasand?uid?ow.Thegasescapingtothesea?oormaybeattributedtotheformationofthesedepressions.ItisalsopossiblethattheseareerosionalchannelsastheiraxisisalongtheslopeofBj?rn?yafan.5.Distributionof?uid-?owfeaturesFluid-?owfeatures,shallowgasaccumulations,andassociatedgashydratesarecharacterizedfromdifferentpartsoftheSWBarentsSea(e.g.Andreassenetal.,1990;LabergandAndreassen,1996).Fluid-?owfeatures,especiallylargegaschimneys,arehy-drocarbonmigrationpathwaysandthelocationofthesefeaturesisimportantforthehydrocarbonindustry(Heggland,1998)sincethesechimneyscouldposeadrillinghazardduetohighpore-?uidpressuresthatmaybepresent(L?sethetal.,2002).Ourstudyshowsthatthe?uid?owisabundantandwidespreadintheSWBarentsSea(Fig.7).216S.Vadakkepuliyambattaetal./MarineandPetroleumGeology43(精彩内容，尽在百度攻略：Figure6.a)Avertical,narrowzoneof?uidleakagefromthesouthernpartoftheBjarmelandPlatformnorthoftheNysleppFaultComplex.Theleakagezoneisapproximately800mwide,whichisinterpretedasaseepagepipe.b)Showschaoticseismicre?ectors,andhighamplitudere?ectorfromthecentralpartoftheFinnmarkPlatform,suggestingmigrationof?uids.Adepression,approximately600mwide,isalsovisibleabovethe?uidmigrationfeature.Thedownwardbendingre?ectorsindicateacousticpull-downduetolow-velocitymaterial,probablygas.c)Cross-cuttinghigh-amplitudere?ectorsassociatedwiththegaschimneyfromtheBj?rn?yrennaFaultComplex.Hugeregionofmaskedacousticre?ectionsandpolarityreversedhigh-amplitudeanomaliesshow?uid?owandgasaccumulation.Thepatchy,crosscuttinghigh-amplitudere?ectormimicsthesea?oorandisinterpretedasthebaseofgashydratestabilityzone.d)Seismicpro?lefromtheBj?rn?yafanshowingpockmark-likedepressionsandassociatedhighamplitudefeeders.Thedepressionswerefewhundredmetersacross.Acousticpull-downandpresenceofbrightspotssuggestthepresenceofgas.Gaschimneysarethemostcommon?uid-?owfeatureinthestudyareaandappearinmostpartswithvarioussizesandshapes.TheRingvass?y-LoppaandBj?rn?yrennaFaultComplexes,northernpartoftheTroms?Basin,thePolheimSub-platformandtheVeslem?yHighshowadistinctlyhigherdensityofgaschimneyscomparedtootherregionsintheSWBarentsSea.FewergaschimneysarepresentintheTroms?Basinandtheeasternpartofthestudyarea,especiallytheFinnmarkPlatform,NordkappBasinandtheBjarmelandPlatform.TheLoppaHighandtheheavilyfaultedareasarounditalsoshowahighconcentrationofgaschimneys.精彩内容，尽在百度攻略：InS.Vadakkepuliyambattaetal./MarineandPetroleumGeology43(217Figure7.MapshowingthedistributionofgaschimneysandleakagealongfaultsintheSWBarentsSea.Theblacklinesarethemajorfaultboundaries.Mostofthefeatureswerelocatedrightontopofmajorfaultsinthearea.精彩内容，尽在百度攻略：theHammerfestBasin,gaschimneysarepresentclosetotheSn?hvitreservoir.Manyofthegaschimneyswerelocatedrightabovemajorfaultsinthestudyarea(Fig.7).S?rvestsnagetBasinshowsmanygaschimneys,whicharenotrelatedtoanymajorfaults.However,theyaresmallandwidelydistributed.LeakagesalongfaultsarepresentinalmostallpartsoftheSWBarentsSea.Theirdensity,however,washigherinthewesternpart,especiallyintheLoppahighandareassurroundingit.RLFCandBFCshowhighconcentrationsofleakagealongfaults.Themajorfaultboundariesbetweendifferentbasinsalsoshownumerousfaultleakages(Fig.7).Ourobservationsindicatethatthe?uidleakagesaremainlyrelatedtomajorfaultsinthearea.Althoughthedistributionofseismicdatausedforthestudyisuneven,thewesternpartofthestudyareaclearlyshowsahigherconcentrationof?uid-?owfeatures.Thiscanbeattributedtovariousreasons.Presenceofhighnumberoffaultsinthewesternpartincreasestheoddsof?uid?owsincefaultreactivationduringupliftandglacialcyclescouldnegativelyaffectthesealingability.TheupperJurassic,TriassicandPermian/Carboniferoussourcerocksareoilmatureinthewesternpartandcanexsolvegasduringupliftanderosion(Ohmetal.,2008).Triassicsourcerocksareover-matureorgas-matureinthewesternpartofSWBarentsSea(Ohmetal.,2008).Inaddition,evaporitesintheeasternpartofthestudyareamighthavenegativelyaffectedhydrocarbonmigrationtotheshallowstrata(DoréandJensen,1996).6.Large?uid-?owfeatures精彩内容，尽在百度攻略：Thehighdensityof2Dseismicpro?lesinsomeareasallowedustomaptheaerialextentofsomeofthe?uid-?owfeaturesintheSWBarentsSea.Thesizeandshapeofthesefeaturesareapproximate,sincetheyarederivedfrom2Ddata.AreassuchastheLoppaHigh,northernpartofHammerfestBasin,northernpartofTroms?BasinandtheRLFChavegoodcoverageof2Dseismicdata,whichallowedthemappingoflargefeaturesintheselocations.Inall,93large?uid-?owfeaturesweremapped(Fig.8).Theyhavepeculiarshapesandcoverhugeareas.Mostofthemterminateintheshallowstrata,withhighamplitudere?ectionsattheircrest,suggestingshallowgasaccumulation.Theareacoveredbytheselarge?uid-?owfeaturesvariedfrom1to600km2.Ofthe93largefeaturesmapped,81%werecomparativelysmallerinarea,varyingfrom1to50km2.Thelargestmapped?uid-?owfeatureisagaschimney,locatedontheRLFCandnorthernpartofTroms?Basin,coveringapproximately600km2.Thetotalareacoveredbytheselarge?uid-?owfeaturesisapproximately3000km2,whichisapproximatelyonepercentoftheSWBarentsSea.Theshapeofthesefeaturesvarieswidelyfromcirculartoelongate.Elongated?uid-?owfeaturesareseenlocatedabovemajorfaults,whilecir-cular?uid-?owfeaturesarepresentonallparts.TheRingvass?y-LoppaandBj?rn?yrennaFaultComplexes,thenorthernpartoftheTroms?Basin,thePolheimSub-platform,andtheVeslem?yHighcontainmostofthelarge?uid-?owfeatures.S?rvestsnagetBasinandFinnmarkPlatformshowfewsmall?uid-?owfeatures.TheVeslem?yHighhasadenserdistributionof?uid-?owfeatures.Thesefeaturesarealsolargerthaninotherareasandmostlyoccurabovemajorfaultboundaries.ThenorthernpartofTroms?Basin,devoidofsaltdomes,alsoshowslarge?uid-?owfeaturesespeciallyalongtheboundarieswithVeslem?yHigh,LoppaHighandPolheimSub-Platform.TheHammerfestBasinshowslarge?uid-?owfeaturesclosetotheSn?hvitreservoirandonitsboundarywiththeLoppaHigh.TheBj?rn?yaBasinshowstwoofthelargest?uid-?owfeatures,covering260km2精彩内容，尽在百度攻略：and218S.Vadakkepuliyambattaetal./MarineandPetroleumGeology43(精彩内容，尽在百度攻略：Figure8.Distributionoflarge?uid?owfeaturesinthearea.Theyvaryinareafromw1kmtow600km2.Histogramplotofareacoveredbytheselargefeaturesshow81%ofthemfallinginthecategorywithanareaof1e50km2.200km2,abovetheBjorn?yrennaFaultComplex.TheLoppaHighshowsaverylargegaschimneyonthenorthernpart,whichcoversanareaof290km2.Thelargest?uid-?owfeatureintheeasternpartofthestudyareaislocatedabovetheSamsonDomeandcovers150km2.TheNordkappBasinshowsnolarge?uid-?owfeatures.7.DiscussionWeobservedsubsurface?uid-?owsystemsonallpartsoftheSWBarentsSea.Theobservedfeatureswereofvarioustypes,interpretedasgaschimneys,leakagealongfaultsandfracturesandotherrelatedfeatures.However,gaschimneysweredominantinmostpartsofthestudyarea(Fig.7).Awidevarietyof?uid-?owexpressionsprobablyindicatesthevariableresponsetoglacialcycles,upliftanderosioninthedifferentbasins.Fluid-?owfeaturesarespatiallyrelatedtothestructuralelementsofthestudyarea,especiallywithfaults(Fig.7)separatingthemajorbasinsandplat-formintheSWBarentsSea.Mostofthe?uid-?owfeatureswerelocatedabovemajordeep-seatedfaultslocatedinhydrocarbon-richsource/reservoirrocksinthestudyarea.Fluid?owalongfaultsisalsowidespreadinthestudyarea(Figs.5and7).Faultsandfracturescanactasmigrationpathwaysfor?uidssincetheyaregenerallymorepermeablethanthesurroundingrock(Berndtetal.,2003;Cartwrightetal.,2007).Removalofsedimentaryoverburdenduringupliftanderosion,andtheconsequentdecreaseinpressure,willcausethegasinagasaccumulationtoexpand.Theeffectofthisexpansion,assumingthatthepre-existingstructurewas?lledtospill,willbetheexpulsionofhydrocarbonsfromtheclosure.Thiswillresultinshorteroillegsand/oralessdense,andhencesmaller,gasaccumulation(c.f.Nylandetal.,1992).Thesameeffectcouldoccurduringrepeatedloadingandunloadingofglaciers(Lerche精彩内容，尽在百度攻略：etal.,1997).Thusglacialcycles,isostaticuplift,anderosionduringtheCenozoiccanberesponsibleforthemajorityofthe?uidleakageobservedthroughouttheSWBarentsSea.NeartheLoppaHigh,wherelarge?uid-?owfeaturesareconcentrated,itisevidentthattheleakageisalongtherotatedfaultblocks(Fig.4a),whichmighthavebeenreactivatedduringglacialcycles.Theserotatedfaultblockscontainoneoftheproli?creser-voirrocksoftheBarentsSea,theSt?formation.TheSnaddfor-mationwithshaleandsandstoneinter-beddingcouldalsobeasourceforhydrocarbonsinthisarea.Fracturingofthecaprockcanbeamajorcauseof?uidleakage(Arntsenetal.,2007),whichcouldbethereasonfor?uidleakageintheSamsonDome(Fig.4c).Suddenreleaseofpressurefromahighlypressurized?uidaccu-mulationcouldhaveresultedintheformationofseepagepipeintheBjarmelandPlatform(Fig.6a)(L?sethetal.,2011;Cartwrightetal.,2007).Structuraltraps,especiallyfaults,arethoughttobehighlysensitivetotheeffectsofupliftanderosion(Henriksenetal.,2011).Extensionalfault-dominatedareassuchastheHammerfestBasin,LoppaHighandVeslem?yHighshowedahighdensityof?uid-?owfeatures.Salt-relatedstructuraltraps,whichareconsideredstableagainstconsiderableamountsofupliftanderosion,presentintheNordkappandTroms?basinsshowedrela-tivelyless?uid-?owfeatures.However,numeroussmallgaschimneysoccuralongthesouthernandwesternrimsoftheNordkappBasin(Fig.7).Thus,thestructuralevolutionofSWBarentsSeamighthaveplayedamajorroleinthe?uid?owhistoryofthearea.Thelarge?uid-?owfeaturesrepresentsigni?cantareasofhy-drocarbonleakage.Manyofthelargestoneswerelocatedclosetothetwomajorfaultcomplexesinthearea,RLFCandBFC.Large?uid-?owzonessuggestunfocussedmigrationofgasfrom精彩内容，尽在百度攻略：theS.Vadakkepuliyambattaetal./MarineandPetroleumGeology43(219精彩内容，尽在百度攻略：Figure9.Theamountofneterosion(blacklines,afterHenriksenetal.,2011)doesnotseemtoaffectthedistributionof?uid?ow(inpink).rotatedfaultblocks,whichcouldprovidemultiplepointsofhy-drocarbonspillage.Suchextensiveareasofleakagesuggestthepresenceofsigni?canthydrocarbonreservoirsinthesubsurface.Someofthe?uidsfromthesereservoirshaveclearlyleakedfromtraps.Therestill,however,maybeeconomicquantitiesofhydro-carbonbeneaththese?uid-leakageareas,asevidencedbydiscov-eriesintheSn?hvitandGoliat?eldsinHammerfestBasin(Doré,1995).Thesourceoftheobserved?uid-?owfeatureswasdif?culttoidentifyfromseismicdataduetotheirdeeporiginandacousticmaskingcausedbyupwardmigratinggas.ThetentativematurityofvarioussourcerocksintheNorwegianBarentsSeasuggestedbyOhmetal.(2008)showsoilmatureupperJurassicHekkingenFormationintheHammerfestbasinandthenorthernpartoftheLoppaHigh.TriassicandPermian/Carboniferousformations(Snadd,Havert)areoilmatureinmajorbasinsintheSWBarentsSeaincludingtheHammerfestBasin.Thepresenceofmultiplesourcerocks,especiallyinthewesternpartofstudyarea,increasesthechanceofhydrocarbongenerationanddissolutionofgasfromoilandcanalsocontributetomixingofhydrocarbonsfromdifferentstrat-igraphicintervals,asobservedinsomewells(e.g.,,Goliatoilwell)intheBarentsSea(Ohmetal.,2008).精彩内容，尽在百度攻略：IsostaticupliftandassociatederosionisconsideredtohaveaffectedthehydrocarbonaccumulationandmigrationintheSWBarentsSea.Manyworkers(Vorrenetal.,1991;Riis,1992;Nylandetal.,1992;Henriksenetal.,2011)havediscussedneterosionintheBarentsSea.Theirstudiessuggestneterosionvaluesofapproximately900e2000mintheSWBarentsSeaandconcludethatdifferentamountsofupliftanderosionintheareacouldaffectthepetroleumsystems.WecorrelatedtheneterosionoftheSWBarentsSea(Henriksenetal.,2011)withthedistributionof?uid-?owfeatures.Wecouldnot?ndanyrelationbetweentheamountofneterosionandthedistributionof?uid-?owfeatures(Fig.9).Theareaswithadensedistributionof?uid-?owfeaturesinthewesternhalfofthestudyareashowanerosionofapproxi-mately1000m,whereastheeasternhalf,withaneterosionofaround2000m,showscomparativelyless?uid-?owfeatures.Thissuggeststhatthe?uidleakageinthestudyareaisprimarilycontrolledbythepresenceofmaturesourcerocksandstructuraltraps,especiallyfaults.Tectonicfaultingandfracturingisoftensuggestedasthecontrollingmechanismforthelocationanddis-tributionof?uid-?owobservationsworldwide(Gayetal.,2007;Barnesetal.,2010;Talukderetal.,2003).Inthewesternpartofthestudyarea,mostofthe?uid-?owfeaturesterminateinyoungersediments(lateTertiary-Quaternary)(Figs.4,5c,6c,andd)whichsuggeststhattheymighthavebeentriggeredbyupliftandglacia-tionsduringthelatePlioceneePleistocene.精彩内容，尽在百度攻略：Gaschimneysterminateatdifferentstratigraphiclevelsinthestudyarea(Figs.4e6).Thissuggeststhatthetimingof?uid?owcouldbedifferentfrombasintobasin.However,regionaltectonicevents,suchasrifting,upliftorglaciationswouldaffectthewholeregionandcouldtrigger?uidleakageatthesametimeregionally.Differenceinthelithologyofshallowsedimentsintheareacouldcausedifferentterminationpointforchimneys,eventhoughthesametectoniceventtriggeredthem.SincethestructuralevolutionoftheSWBarentsSeaiscomplexanddifferentfrombasintobasin,amorefocusedstudyonindividualbasinsmaybeneededtoaccuratelyanalyzetheoriginandtimingofthese?uid-?owfeatures.8.ConclusionsFluid?owisabundantandwidespreadintheSWBarentsSeawithsomeverylargegaschimneyscoveringapproximately精彩内容，尽在百度攻略：one220S.Vadakkepuliyambattaetal./MarineandPetroleumGeology43(percentofthestudyarea.Differenttypesof?uid-?owfeaturesoccurinthearea,themostdominantbeinggaschimneys.Thedistributionof?uid-?owfeaturesshowedadirectrelationshipwiththestructuralsettingoftheSWBarentsSea.Thiscouldbeduetotheinabilityofdeep-seatedfaultstoeffectivelysealthetrappedhydrocarbons.Faulttrapscouldbehighlysensitivetotheeffectsofuplift,erosionandglaciations.The?uid-?owfea-tureswerehighlydenseinthewesternpartoftheSWBarentsSea.Thedifferenceindistributioncouldbeduetoa)presenceofmultiplesourcerocks,whichareover-matureorgasmatureinthewesternpart,b)availabilityofstructuraltraps,especiallyfaultsandc)presenceofevaporitesintheeasternpart.Theamountofneterosioninthestudyareadidnotseemtobecontrollingthedistributionof?uidleakagefeatures.Giventherelationof?uid?owtothestructuralsetting,extensionaltec-tonics,upliftandglaciationsinthePlio-Pleistocenetimecouldhaveplayedmajorrolesinthetimingandactivityofthe?uidleakage,althougherosionmighthavehadanaddedeffect.However,duetothestructuralcomplexityofthestudyareaandthenumberof?uid-?owfeaturesobserved,amorefocusedstudyonthetimingandoriginof?uid-?owfeaturesinindi-vidualbasinsisnecessary.Acknowledgments精彩内容，尽在百度攻略：TheauthorsarethankfultoTGS-NOPECGeophysicalCompanyforprovidingsomeoftheseismicdata.WethankSchlumbergerforprovidingthePetrelInterpretationsoftware.WearegratefultoAndrewSmithforcorrectingtheEnglishlanguage.ReviewsbyMartinHovlandandHeraldLigtenbergsigni?cantlyimprovedthemanuscript.ReferencesAguilera,R.,1995.NaturallyFracturedReservoirs,seconded.PennWell,Tulsa,OK.Andreassen,K.,Hogstad,K.,Berteussen,K.A.,1990.GashydrateinthesouthernBarentsSea,indicatedbyashallowseismicanomaly.FirstBreak8,235e245.Andreassen,K.,Nilssen,E.,?degaard,C.,2007a.Analysisofshallowgasand?uid精彩内容，尽在百度攻略：migrationwithinthePlio-PleistocenesedimentarysuccessionoftheSWBarentsSeacontinentalmarginusing3Dseismicdata.Geo-MarineLetters27,155e171.Andreassen,K.,?degaard,C.M.,Rafaelsen,B.,2007b.Imprintsofformericestreamsimagedandinterpretedusingindustrythree-dimensionalseismicdatafromthesouth-westernBarentsSea.In:GeologicalSociety,London,SpecialPubli-cations,vol.277,pp.151e169.精彩内容，尽在百度攻略：Anell,I.,Thybo,H.,Artemieva,I.M.,2009.CenozoicupliftandsubsidenceintheNorthAtlanticregion:geologicalevidencerevisited.Tectonophysics474,78e105.Arntsen,B.,Wensaas,L.,Loseth,H.,Hermanrud,C.,2007.Seismicmodelingofgas精彩内容，尽在百度攻略：chimneys.Geophysics72,Sm251eSm259.Berglund,L.T.,Augustson,J.,F?rseth,R.,Gjelberg,I.,Ramberg-Moe,H.,1986.TheevolutionoftheHammerfestBasin.In:Spencer,A.M.,etal.(Eds.),HabitatofHydrocarbonsontheNorwegianContinentalShelf:ProceedingsofanInter-nationalConference(HabitatofHydrocarbons,NorwegianOilandGasFinds).Graham&TrotmanfortheNorwegianPetroliumSociety,London,pp.319e338.Barnes,P.M.,Lamarche,G.,Bialas,J.,Henrys,S.,Pecher,I.,Netzeband,G.L.,精彩内容，尽在百度攻略：Greinert,J.,Mountjoy,J.J.,Pedley,K.,Crutchley,G.,2010.TectonicandgeologicalframeworkforgashydratesandcoldseepsontheHikurangisubductionmargin,NewZealand.MarineGeology272,26e48.Berndt,C.,Bünz,S.,Mienert,J.,2003.Polygonalfaultsystemsonthemid-Norwegianmargin:along-termsourcefor?uid?ow.In:GeologicalSociety,London,SpecialPublications,vol.216,pp.283e290.精彩内容，尽在百度攻略：Bjor?y,M.,Hall,P.B.,Ferriday,I.L.,M?rk,A.,2009.TriassicSourceRocksoftheBarentsSeaandSvalbard.AAPGConvention,Denver,Colorado,USA.Bj?rkum,P.A.,Walderhaug,O.,Nadeau,P.H.,2001.Thermallydrivenporosity精彩内容，尽在百度攻略：reduction:impactonbasinsubsidence.In:GeologicalSociety,London,SpecialPublications,vol.188,pp.385e392.Brekke,H.,Riis,F.,1987.TectonicsandBasinEvolutionoftheNorwegianShelfBetween62-Degrees-Nand72-Degrees-N.In:NorskGeolTidsskr,vol.67.pp.295e321.精彩内容，尽在百度攻略：Carstens,H.,2005.Gasfoundinglacial,shallowsands.GeoExPro,GeoscienceandTechnologyExplained4,24e25.Cartwright,J.,Huuse,M.,Aplin,A.,2007.Sealbypasssystems.AapgBulletin91,精彩内容，尽在百度攻略：.Cavanagh,A.J.,DiPrimio,R.,Scheck-Wenderoth,M.,Hors?eld,B.,2006.SeverityandtimingofCenozoicexhumationinthesouthwesternBarentsSea.JournaloftheGeologicalSociety,London163,761e774.精彩内容，尽在百度攻略：Chand,S.,Mienert,J.,Andreassen,K.,Knies,J.,Plassen,L.,Fotland,B.,2008.GashydratestabilityzonemodellinginareasofsalttectonicsandpockmarksoftheBarentsSeasuggestsanactivehydrocarbonventingsystem.MarineandPetroleumGeology25,625e636.Chand,S.,Rise,L.,Ottesen,D.,Dolan,M.F.J.,Bellec,V.,B?e,R.,2009.Pockmark-like精彩内容，尽在百度攻略：depressionsneartheGoliathydrocarbon?eld,BarentsSea:morphologyandgenesis.MarineandPetroleumGeology26,.Chand,S.,Thorsnes,T.,Rise,L.,Brunstad,H.,Stoddart,D.,B?e,R.,L?gstad,P.,Svolsbru,T.,2012.Multipleepisodesof?uid?owintheSWBarentsSea(LoppaHigh)evidencedbygas?ares,pockmarksandgashydrateaccumulation.EarthandPlanetaryScienceLetters331e332,305e314.精彩内容，尽在百度攻略：Connolly,D.L.,Brouwer,F.,Walraven,D.,2008.Detectingfault-relatedhydrocarbonmigrationpathwaysinseismicdata:implicationsforfault-seal,pressure,andchargeprediction.GulfCoastAssociationofGeologicalSocietiesTransactions58,191e203.Dahl,B.,Augustson,J.H.,1993.Thein?uenceofTertiaryandQuaternarysedimen-tationanderosiononhydrocarbongenerationintheNorwegianoffshorebasins.In:Doré,A.G.,etal.(Eds.),BasinModeling:AdvancesandApplications.NPFSpecialPublications3.Elsevier,Amsterdam,pp.419e432.精彩内容，尽在百度攻略：Dalland,A.,Worsley,D.,Ofstad,K.,1988.ALithostratigraphicalSchemefortheMesozoicandCenozoicSuccessionOffshoreMid-andNorthernNorway.NorwegianPetroleumDir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