| 松辽盆地龙西地区泉四段砂岩成岩序列及孔隙演化特征 |
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| 引用本文： | 连承波,钟建华,杨玉芳,渠芳,杨军. 松辽盆地龙西地区泉四段砂岩成岩序列及孔隙演化特征[J]. 西安地质学院学报, 2010, 0(2): 155-160 |
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| 作者姓名： | 连承波 钟建华 杨玉芳 渠芳 杨军 |
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| 作者单位： | [1]西南石油大学资源与环境学院,四川成都610500 [2]中国石油大学地球资源与信息学院,山东东营257061 [3]中国科学院广州地球化学研究所,广东广州510640 [4]中国石油天然气集团公司大庆油田有限责任公司勘探开发研究院,黑龙江大庆163712 |
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| 基金项目： | 中国石油天然气集团公司创新基金项目（2002F70108） |
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| 摘 要： | 通过岩芯观察、镜下薄片、扫描电镜和X衍射分析等资料,对松辽盆地龙西地区泉四段砂岩的岩石学特征、成岩作用类型、成岩阶段划分和成岩共生序列及孔隙演化特征进行了研究。结果表明：龙西地区泉四段主要为长石质岩屑砂岩,局部为岩屑质长石砂岩;经历的主要成岩作用类型有压实作用、自生石英胶结作用、自生黏土矿物胶结作用、碳酸盐胶结作用、交代和溶蚀作用等;龙西地区泉四段砂岩为中成岩阶段A期,且细分为A1和A2亚期;随着成岩演化,压实和胶结作用使得原生孔隙减小,而溶蚀作用使得储层孔隙结构得到改善;孔隙类型由缩小粒间孔组成变为由缩小粒间孔和溶蚀粒间孔组合组成。
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| 关 键 词： | 成岩序列 孔隙演化 泉四段 龙西地区 松辽盆地 |
Characteristics of Quan-4 Formation Sandstone Diagenetic Sequence and Porosity Evolution in Longxi Area of Songliao Basin |
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| LIAN Cheng-bo,ZHONG Jian-hua,YANG Yu-fang,QU Fang,YANG Jun. Characteristics of Quan-4 Formation Sandstone Diagenetic Sequence and Porosity Evolution in Longxi Area of Songliao Basin[J]. , 2010, 0(2): 155-160 |
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| Authors: | LIAN Cheng-bo ZHONG Jian-hua YANG Yu-fang QU Fang YANG Jun |
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| Affiliation: | 1.School of Resources and Environment,Southwest Petroleum University,Chengdu 610500,Sichuan,China;2.School of Geo-resources and Information,China University of Petroleum,Dongying 257061,Shandong,China;3.Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,Guangdong,China;4.Institute of Exploration and Development,Daqing Oilfield Company,China National Petroleum Corporation,Daqing 163712,Heilongjiang,China) |
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| Abstract: | Based on core,cast thin section,scanning electron microscope,X-ray diffraction and so on,the characteristics of petrology,types of diagenesis,division of diagenetic stage,diagenetic concordant sequence and porosity evolution in Quan-4 Formation sandstone in Longxi area of Songliao Basin are studied.The results show that the lithology is mainly feldspathic litharenite,and secondly lithic arkose;types of diagenesis are compaction,authigenic quartz cementation,authigenic clay mineral cementation,carbonate cementation,metasomatism and dissolution;the diagenetic stage in Quan-4 Formation is A period mesogenetic stage,and divided into A1 and A2 substages;diagenetic,compaction and cementation decrease the primary pore structure intensively,however dissolution improves it effectively;pore type is changed from reduced intergranular pore into combination of reduced intergranular pore and corrosion intergranular pore gradually because of diagenetic evolution. |
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| Keywords: | diagenetic sequence porosity evolution Quan-4 Formation Longxi area Songliao Basin |
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