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鄂尔多斯古生界流体包裹体特征及其与油气演化关系
引用本文:刘德良,谈迎,孙先如,李振生,方国庆,陶士振.鄂尔多斯古生界流体包裹体特征及其与油气演化关系[J].沉积学报,2002,20(4):695-704.
作者姓名:刘德良  谈迎  孙先如  李振生  方国庆  陶士振
作者单位:1 中国科学技术大学地球与空间科学学院,合肥,230026;
基金项目:国家科技攻关项目,国家自然科学基金,0102016j02,40172072,,
摘    要:对鄂尔多斯盆地奥陶系碳酸盐岩、石炭-二叠系石英砂岩成岩作用研究的基础上,分别对上述岩石流体包裹体作了初步研究。奥陶系碳酸盐岩包裹体均一温度具有三个区段 :6 0~ 10 0℃,10 0~ 16 0℃,16 0~ 2 2 0℃;石炭-二叠系石英砂岩包裹体均一温度三个区段为 90~ 110℃,12 0~ 14 0℃,16 0~ 2 2 0℃。并利用包裹体测温资料结合已有的镜质体反射率、磷灰石裂变径迹等研究成果,对流体包裹体在鄂尔多斯盆地油气田形成、演化中应用作了初步探讨。

关 键 词:成岩作用    流体包裹体    古生界    鄂尔多斯盆地
文章编号:1000-0550(2002)04-0695-10
收稿时间:2001-07-11
修稿时间:2001年7月11日

Characteristics of Erathem Fluid Inclusions and Their Relationship with Oil-gas Evolution in Ordos Basin
LIU De liang TAN Ying SUN Xian ru LI Zheng sheng FANG Guo qing , TAO Shi zheng.Characteristics of Erathem Fluid Inclusions and Their Relationship with Oil-gas Evolution in Ordos Basin[J].Acta Sedimentologica Sinica,2002,20(4):695-704.
Authors:LIU De liang TAN Ying SUN Xian ru LI Zheng sheng FANG Guo qing  TAO Shi zheng
Institution:1 College of Earth and Space Science,USTC,Hefei 230026;2 Anhui Institute of Geology, Hefei 230001;3 Lanzhou Institute of Geology,CAS, Lanzhou 730000;4 Petroleum Exploration and Development Institute CNPC, Beijing 100083
Abstract:On the base of research on diagenesis of Ordovivian carbonati te and quartzose sandstone in Ordos basin, preliminary S tudy on inclusio ns in these rocks have been done.There are three sections of homgogenization temperature of inclusio ns in Ordovician carbonate rock :60 ℃~ 100 ℃, 100 ℃~ 160 ℃, 160 ℃~ 220 ℃;and there are three sections of homogenization temperature of inclusions in Permocarboniferous quartzose;90 ℃~ 110 ℃, 120 ℃~140 ℃, 160 ℃~ 220℃.Making use of temperature data of inclusions combined w ith the recently research result of vitrinite reflectivity and apatite fission track, the paper discussed the application of fluid inclusions to formation and evolution of oil-gas reservoirs in Ordos basin.
Keywords:fluid inclusion    diagencesis    Erathem    Ordos basin
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