简介：通过对尕斯库勒砂西区块N1—N21油藏Ⅺ、Ⅹ—Ⅸ、Ⅷ—Ⅵ、Ⅴ—Ⅰ油层组段沉积相特征、沉积体系展布及演化规律的综合分析,认为砂西区块N1—N21油藏从下向上发育滨浅湖亚相、辫状河三角洲前缘-滨浅湖亚相、辫状河三角洲平原-前缘亚相,整体为一套反旋回沉积.在此基础上分析了砂西区块N1—N21油藏沉积相与油气分布的关系.结果表明,分布于Ⅷ—Ⅵ油层组的辫状河三角洲分流河道及构造高部位的河口坝、远砂坝微相砂体为该地区的主要储集体,Ⅴ—Ⅰ油层组发育的泛滥平原微相泥岩为该区的区域性盖层.

简介：<正>ONSOUTHERNSTRETCHOPTHES-NTECTONICBELT,CHINAChenGuanghaoandWeiZhoulin(ChangshaInstituteofGeotectonic,AcademiaSinica,Changsha,410013,Hunan,China)S-Ntectonicbelt,southstretching,boundingbeltItcanbeinferredfromthegeophysicaldata,linearstructures,tectonicevolu-tionhistoryandmetallogenythattheS-NtectonicBeltstretchesfurthersouthinadifferentdi-rectionandmannerafterinterceptedbytheRedRiverFault,Thestretchingsegmentistheim-portanttectonicboundaryinIndo-AsiaandassiminlatestheS-Ntectonicbeltwithsomediffer-ences.

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简介：TheJiamusimcdianmassifislocatcdaboutlittlcXinganlingtoLaoycling,casternHeilongjiangProvince.Beinginaccordwiththediwathcory,thcJiamusipalaco-mcdianmassifdevclopspre-geosyn-clinlarchacansialiccrust.KhondalitescricsinthcJiXidistrictmaybcrcputcdasrcprcscntivc,isotopicageofwbichis25OOMa.ThcrcarethcDongfc

简介：这研究在Balong提供n链烷和Holocene黄土的花粉记录()镇，Dulan()县，Qinghai()省，和环境变化从同意很好的两个记录重建了。过去的气候变化的三个阶段被n链烷和花粉代理的变化译解。在5370一BP前，气候温暖干燥却稍微潮湿，相应于Mid-Holocene气候的最佳；53703830一BP，气候或者变化了在之间温暖干燥稍微潮湿、温暖干燥，从Mid-Holocene气候的最佳显示转变到迟了的Holocene冷时期；在3830一BP以后，气候主要是温暖干燥的。温暖的凉爽、极其干燥的气候被n链烷和花粉代理在30402600一BP期间记录，建议环境演变为荒芜或咸的湖，根据在西方的周王朝的冷、高度经常的自然灾难时期(ca。29962721一BP)在中国。

简介：ObjectiveThenearlyparallelN–S-trendingriftsinsouthernTibetrepresenttheE–WextensionoftheTibetPlateau.MostdatawhichconstrainedtheageoftheextensionaldeformationcomefromisotopicdatingofthedikesprobablyrelatedtotheactivityofthenearlyN–Sfaultingandmicasfromhydrothermalactivityandthelowtemperaturethermochronologyofplateauuplift.Previous

简介：ThetransitionzonebetweentheEastAsiaandCentralAsiacrustobodlesisnotonlyadiwaregion,butalsoagigantictectono-metallogenicbeltinAsia.IttrendsN-S,liesbetweenlong.100°-107°Eandlat.14°-62°N,hasalengthof4600kmandfurtherextendssouthwardandnorthward.Themainfeaturesofthebeltareasfollows:(1)Thebc1tcon8istsofotc