塔里木盆地北部深层风化壳储层的形成与分布

朱光有, 张水昌, 王欢欢, 杨海军, 孟书翠, 顾乔元, 张斌, 苏劲. 塔里木盆地北部深层风化壳储层的形成与分布[J]. 岩石学报, 2009, 25(10): 2384-2398.
引用本文: 朱光有, 张水昌, 王欢欢, 杨海军, 孟书翠, 顾乔元, 张斌, 苏劲. 塔里木盆地北部深层风化壳储层的形成与分布[J]. 岩石学报, 2009, 25(10): 2384-2398.
ZHU GuangYou, ZHANG ShuiChang, WANG HuanHuan, YANG HaiJun, MENG ShuCui, GU QiaoYuan, ZHANG Bin, SU Jin. The formation and distribution of deep weathering crust in north Tarim Basin[J]. Acta Petrologica Sinica, 2009, 25(10): 2384-2398.
Citation: ZHU GuangYou, ZHANG ShuiChang, WANG HuanHuan, YANG HaiJun, MENG ShuCui, GU QiaoYuan, ZHANG Bin, SU Jin. The formation and distribution of deep weathering crust in north Tarim Basin[J]. Acta Petrologica Sinica, 2009, 25(10): 2384-2398.

塔里木盆地北部深层风化壳储层的形成与分布

  • 基金项目:

    国家自然科学基金项目(批准号:40602016)、国家重点基础研究发展计划项目(项目编号:113404GJ0003)和中国石油科技研究项目《油气勘探新领域、新理论、新方法研究--深层油气地质与勘探潜力研究》资助

The formation and distribution of deep weathering crust in north Tarim Basin

  • 塔北地区碳酸盐岩风化壳岩溶储层发育,储层具有质量好、分布面积广、埋藏深等特点,并已在轮南、塔河和英买力等地区发现数个亿吨级规模以上的大型油气田。本文通过对塔北地区200多口重要井的钻井、录井、测井、试油等第一手资料的系统分析,结合大量的分析化验资料与岩心及镜下观察,精细研究了风化壳储层的成因特点、分布规律与评价预测等。研究认为,寒武系发育白云岩型风化壳储层,以孔洞型储层为主; 奥陶系主要为灰岩型风化壳储层,储层的基质孔隙度较低,溶蚀孔洞、溶蚀扩大缝和构造缝是其主要的储集空间,储层以洞穴型储层和网状裂缝型储层为主。台地相发育的纯净碳酸盐岩、海西期构造运动导致地层的长期暴露剥蚀、断裂裂隙作用和晚期大气淡水淋溶等是控制塔北风化壳储层形成的的重要因素; 并发现塔北地区风化侵蚀能够作用到的深度主要在140m以内。虽然风化壳储层基质孔隙较差,但是储层物性受埋深影响不大; 在有利的古岩溶地貌和断裂发育区,即使在更大的埋藏深度,也可能发育规模较大、性能较好的储集体。
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刊出日期:  2009-10-31

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