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Determination of Salinity in Fluid Inclusions with Laser Raman Spectroscopy Technique 总被引:2,自引:0,他引:2
Seyed Javad Moghaddasi 《中国地质大学学报(英文版)》2000,11(4)
INTRODUCTIONLaserRamanmicroprobehasbeenfoundinmanygeologicalapplications (Shovaletal.,1995 ;McMillanandHofmeister,1988;McMillan ,1984;Dubessyetal.,1982 ;Griffith ,1975 )andasanon destructiveandinsitutechnique,ithashadatremendousimpactondevelopmentoffluidinclusioncomposi… 相似文献
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Liu Shaofeng Department of Geology Northwest University Xi’an Li Sitian Yang Shigong Cheng ShoutianFaculty of Earth Resources China University of Geosciences Wuhan 《中国地质大学学报(英文版)》1997,(1)
EarlyMesozoicBasin┐MountainCouplingMechanismandBasinGeodynamicsofEastChina*LiuShaofengDepartmentofGeology,NorthwestUniversity... 相似文献
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Chen Nengsong Zhang Kexin Wang Guocan Hou Guangjiu Zhu Yunhai Faculty of Earth Sciences China University of Geosciences Wuhan 《中国地质大学学报(英文版)》1998,9(3)
TheCentralMountainRangesofChina,whichocupythecentralpartofChina,comprisemainlytheDabieMoun-tainsintheeast,theQinlingMountains... 相似文献
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Zhao Xingmin Wu Bihao Institute of Mineral Deposits Chinese Academy of Geological Sciences Beijing Wang Yaping Experimental Institute Chinese Academy of Geological Sciences Beijing Lu Zhenquan Institute of Mineral Deposits Chine 《中国地质大学学报(英文版)》2000,11(4)
Madeupofwaterandmethane,gashydratesareice likeclathratecompoundsthatformedintheconditionsoflowtempera ture (0 - 10℃ )andhighpressure (>10MPa) (MaxandDillon ,1998) .Generallyspeaking,theyarealsocalledmethanehydratesbecausemethaneisadominantcomposition .Besidesmethane,… 相似文献
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Fei Anwei Zhang Zhongtao Resources Information Institute University of Petroleum Beijing 《中国地质大学学报(英文版)》2002,13(4)
INTRODUCTIONThestudyareaislocatedinthesoutheasternmar ginoftheOrdosbasinandliesintheFupingzoneofShaanxiProvince ,China .ThestudyintervaliswithintheBadouMemberofFengfengFormationandtheMember 1ofJinsushanFormation ,whichhavebeenclassifiedastheMiddleOrdovic… 相似文献
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澳大利亚矿业管理体制及其启示 总被引:2,自引:0,他引:2
澳大利亚矿业管理体制及其启示明晓寰江苏省地质矿产局,南京,210018关键词:矿业管理,矿业权,矿产资源,环境保护,澳大利亚ManagementSystemandInspirationstoAustralianMiningIndustry¥MingX... 相似文献
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BGHMS:AGeohistoryModelingSystemforCratonicBasinsYeJiaren;LuMingd;WangFeiqiao(DepartmentofPetroleumGeology,ChinaUniversityofGe... 相似文献
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湖南地矿行政管理工作现状及今后工作思路的探讨①PresentSituationofAdministrativeManagementofHunanGeologyandMineralResourcesandInvestigationontheWorkTh... 相似文献
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NIE Fengjun Institute of Mineral Deposits Chinese Academy of Geological Sciences Beijing China Arne BJRLYKKE Department of Geology University of Oslo P.O.Box Blindern Oslo Norway 《Continental Dynamics》1999,(1)
1-Introduction TheorogenicbeltofInnerMongoliaislocatedbetweentheNorthChinaCratonandtheSiberianPlatform.ThisbeltisconsideredapartoftheCentralAsiaMongoliangeosyncline(IchikawaandWang,1991)orCentralAsianMongolianmobilebelt.ThenorthernlimitoftheNorthC… 相似文献
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Liu Qingsheng Department of Applied Geophysics China University of Geosciences Wuhan Gao Shan Faculty of Earth Sciences China University of Geosciences Wuhan Xu Qidong Faculty of Earth Resources China University of Geosciences W 《中国地质大学学报(英文版)》1998,9(2)
ThepaperissupportedbyNationalNaturalScienceFoundation,NationalEducationCommiteeandMinistryofGeologyandMineralResourcesofChina... 相似文献
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DIAGENESISANDRESERVOIRCHARACTERISTICSOFDOLOSTONESTRATAOFCAMBRIANSYSTEMINJURONGCOUNTY,JIANGSUPROVINCE
《Scientia Geologica Sinica》1998,(3)
1.IntroductionThispaperisoneoftheachievementsofaChineseEightfiveyearPlan’skeyproject.ThefieldworkwascariedoutduringMarchtoMa... 相似文献
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《Scientia Geologica Sinica》1998,(2)
1.IntroductionThesystematictheoryinRockMasEngineeringGeologyistheRockMasEngineeringGeomechanicsestablishedbyGuDezhen(1979).He... 相似文献
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Two-DimensionalModelofHydraulicFracturinginGeosciences:Effects of Fluid BuoyancyYoshitoNakashima;MitsuhiroToriumi(GeologicalI... 相似文献
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通过中国北方5.30Ma以来含丰富哺乳动物化石的典型剖面的磁性地层研究,建立5.30Ma以来中国北方陆相哺乳动物群与磁性地层序列对比。中国黄土记录了Brunhes正极性带与Matuyama负极性带,黄土年龄约2.50MaB.P.,其中发现有午城动物群、公王岭动物群、阳郭动物群、陈家窝动物群与靖远动物群。三门组记录了Matuyama负极性带下段,年龄约1.20—2.50Ma,其中发现有三门动物群。静乐剖面的静乐红土对应于Gauss正极性带上段,年龄约2.50—3.00Ma,其中发现有静乐贺丰动物群。游河组记录了Gauss正极性带,年龄约2.50—3.40Ma,其中发现游河动物群。泥河湾沉积对应于Brunhes正极性带、Matuyama负极性带、Gauss正极性带,年龄约0.13—3.40Ma。其中小长梁剖面记录了Brunhes正极性带与Matuyama负极性带上段(含Jaramilo亚带),年龄约0.13—1.00Ma(其中含化石及石器地层年龄约0.90—1.00Ma)。榆社盆地麻则沟组记录了Gauss正极性带(2.50—3.40Ma),高庄组记录了Gilbert负极性带(3.40—5.30Ma)。 相似文献
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Zavodchikova Maria 《中国地质大学学报(英文版)》1994,(1)
BasicFactsConcerningStrengthofSandstone¥ZavodchikovaMaria(Sankt-PetersburyMiningInstitute,Sankt-Petersburg199026;)(Eepartment... 相似文献
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Barium Anomaly and Its Geochemical Significance 总被引:2,自引:0,他引:2
WANYusheng Institute of Geology Chinese Academy of Geological Sciences Beijing China 《Continental Dynamics》1999,(1)
1.Introduction Multielementvariationdiagramsareveryusefulinthegeochemicalstudy.OneofthemisthePearcediagram,theMORBnormalizedmultielementvariationdiagramgivenbyPearce(1983).ThisdiagramshowstherelativedepletionsofHFSelementsNb,TiandP.Inaddition,the… 相似文献
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《Scientia Geologica Sinica》1998,(1)
AVALIDMETHODTOSTUDYPALEOGEOTEMPERATUREQiuNanshengUniversityofPetroleum,Beijing102200(ReceivedMay15,1997)AbstractThekerogensam... 相似文献