石油学报 ›› 2021, Vol. 42 ›› Issue (1): 15-32.DOI: 10.7623/syxb202101002
宁超众1, 孙龙德2, 胡素云1, 徐怀民3, 潘文庆4, 李勇1, 赵宽志4
收稿日期:
2019-12-24
修回日期:
2020-09-11
出版日期:
2021-01-25
发布日期:
2021-02-05
通讯作者:
宁超众,男,1988年12月生,2012年获中国石油大学(华东)学士学位,2018年获中石油勘探开发研究院博士学位,现为中国石油勘探开发研究院工程师,主要从事油气田开发地质研究。
作者简介:
宁超众,男,1988年12月生,2012年获中国石油大学(华东)学士学位,2018年获中石油勘探开发研究院博士学位,现为中国石油勘探开发研究院工程师,主要从事油气田开发地质研究。Email:nniinngg@petrochina.com.cn
基金资助:
Ning Chaozhong1, Sun Longde2, Hu Suyun1, Xu Huaimin3, Pan Wenqing4, Li Yong1, Zhao Kuanzhi4
Received:
2019-12-24
Revised:
2020-09-11
Online:
2021-01-25
Published:
2021-02-05
摘要: 近年来,塔里木盆地缝洞型碳酸盐岩因持续发现超深层资源潜力而备受关注,但该类储层存在成因和特征不明确以及勘探方向缺乏有效指导等问题。基于地震资料解释,结合资料调研、野外露头考察、岩心及薄片观察、地球化学分析和生产特征分析等手段,对哈拉哈塘地区奥陶系缝洞型碳酸盐岩的岩溶类型和特征进行了深入研究。哈拉哈塘地区发育表生岩溶和热液岩溶两类岩溶储层且特征差异明显。表生岩溶储层主要发育在良里塔格组,在良里塔格组顶面形成典型的岩溶地貌,内部形成水平管状洞穴体系;洞穴发生充填、垮塌和强烈压实,导致储层较致密,储集物性相对较差。热液岩溶储层主要发育在一间房组和鹰山组上部,沿断裂发育形成竖型洞穴,该类型洞穴及其垮塌体保留大量储集空间,在地震剖面上表现为强振幅"串珠",造成频繁的放空和漏失现象,是哈拉哈塘油田奥陶系主要油气储集体。而热液岩溶储层是现阶段研究区勘探开发的主要目标,而表生岩溶储层应合理规避。
中图分类号:
宁超众, 孙龙德, 胡素云, 徐怀民, 潘文庆, 李勇, 赵宽志. 塔里木盆地哈拉哈塘油田奥陶系缝洞型碳酸盐岩储层岩溶类型及特征[J]. 石油学报, 2021, 42(1): 15-32.
Ning Chaozhong, Sun Longde, Hu Suyun, Xu Huaimin, Pan Wenqing, Li Yong, Zhao Kuanzhi. Karst types and characteristics of the Ordovician fracture-cavity type carbonate reservoirs in Halahatang oilfield,Tarim Basin[J]. Acta Petrolei Sinica, 2021, 42(1): 15-32.
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