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塔里木盆地下古生界白云岩储层特征与成因类型
引用本文:焦存礼,邢秀娟,何碧竹,陈代钊,李程成,刘忠宝.塔里木盆地下古生界白云岩储层特征与成因类型[J].中国地质,2011,38(4):1008-1015.
作者姓名:焦存礼  邢秀娟  何碧竹  陈代钊  李程成  刘忠宝
作者单位:1. 中国石油化工股份有限公司石油勘探开发研究院,北京,100083
2. 中国石化国际石油勘探开发有限公司,北京,100083
3. 中国地质科学院地质研究所国土资源部大陆动力学重点实验室,北京,100037
4. 中国科学院地质与地球物理研究所,北京,100029
5. 中原石油勘探局勘察设计研究院,河南濮阳,457001
基金项目:国家重大专项(2008ZX05005-002); 中国石化股份有限公司科技开发部项目(YPH08110)联合资助
摘    要:塔里木盆地寒武系—奥陶系白云岩具有时代老、埋藏深、成岩作用复杂的特点。白云岩储层储集空间主要为孔隙和裂缝两大类,其中孔隙类型可进一步划分为晶间孔、晶间溶孔、晶内溶孔、铸模孔、溶蚀孔洞等;裂缝类型可进一步划分为缝合线、风化裂缝和构造裂缝。根据储集空间类型特征,白云岩储层可以划分为孔隙型、孔洞型、缝洞型和裂缝型4种。孔隙型储层和缝洞型储层物性较好。根据成因白云岩储层可以划分为准同生白云岩储层、埋藏型白云岩储层、构造-热液型白云岩储层和风化壳岩溶型白云岩储层,其中后两者及其复合类型常形成优质储层。

关 键 词:塔里木盆地  寒武系—奥陶系  白云岩  储层类型

Characteristics and genetic types of Cambrian-Ordovician dolomite reservoirs in Tarim basin
JIAO Cun-li,XING Xiu-juan,HE Bi-zhu,CHEN Dai-zhao,LI Cheng-cheng,LIU Zhong-bao.Characteristics and genetic types of Cambrian-Ordovician dolomite reservoirs in Tarim basin[J].Chinese Geology,2011,38(4):1008-1015.
Authors:JIAO Cun-li  XING Xiu-juan  HE Bi-zhu  CHEN Dai-zhao  LI Cheng-cheng  LIU Zhong-bao
Institution:JIAO Cun-li1,XING Xiu-juan2,HE Bi-zhu3,CHEN Dai-zhao4,LI Cheng-cheng5,LIU Zhong-bao1(1.Sinopec Petroleum Exploration & Production Research Institute,Beijing 100083,China,2.Sinopec International Petroleum Exploration and Production Corporation,3.Key Laboratory of Continental Dynamics of Ministry of Land and Resources,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,4.Zhongyuan Engineering Company,Puyang 457001,Henan,China)
Abstract:The Cambrian-Ordovician dolomite in Tarim basin is characterized by old age,deep burial and complex diagenesis.The space of the dolomite reservoir is mainly composed of pores and cracks.The pores can be further divided into such types as intercrystal pores,intercrystal dissolved pores,intracrystal pores,moldic pores and dissolved holes,while the cracks can be further divided into satures,weathering fractures and structural fractures.According to the characteristics of reservoir space,dolomite reservoirs can...
Keywords:dolomite  reservoir classification  Cambrian-Ordvician  Tarim basin  
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