石油与天然气地质 ›› 2023, Vol. 44 ›› Issue (3): 637-650.doi: 10.11743/ogg20230309
侯明才1(), 何小胡2, 金秋月2, 曹海洋1, 贺礼文2, 阙有缘1, 陈安清1
收稿日期:
2023-02-15
修回日期:
2023-03-20
出版日期:
2023-06-01
发布日期:
2023-06-05
通讯作者:
何小胡
E-mail:houmc@cdut.edu.cn
第一作者简介:
侯明才(1968—),男,教授、博士生导师,大地构造沉积学、古地理学、石油地质学。E-mail: 基金项目:
Mingcai HOU1(), Xiaohu HE2, Qiuyue JIN2, Haiyang CAO1, Liwen HE2, Youyuan QUE1, Anqing CHEN1
Received:
2023-02-15
Revised:
2023-03-20
Online:
2023-06-01
Published:
2023-06-05
Contact:
Xiaohu HE
E-mail:houmc@cdut.edu.cn
摘要:
中国海域盆地潜山已成为重要的勘探新领域。琼东南盆地中生代潜山勘探钻揭多个含气构造,但未获得规模性气藏发现。究其原因,储层成因机制和分布规律是制约潜山勘探大发现的瓶颈。基于琼东南盆地已有钻井、岩心、薄片和地球物理资料,研究了琼东南不同构造带潜山储层的发育特征,并探究了潜山储层的成因机制。结果表明:①储集空间主要是构造裂缝,前新生代的印支期和燕山期逆冲挤压构造是成缝关键,相关的先存主断层为潜山分带结构形成奠定了基础,新生代拉张构造活动使先存网状断裂体系活化;②以长英质矿物为主的基岩是最有利的储集岩,多期流体作用有效改造了潜山储层质量,并促成了潜山储层的垂向分带性;③琼东南盆地中生代潜山构造带可划分为南部双层强构造改造型潜山、中部三层风化-构造改造型潜山及北部准单层弱风化改造型潜山;④经历印支期构造活动的老基岩更有利于优质潜山储层发育,邻近凹陷周缘的潜山更有利于形成大型气藏。
中图分类号:
图3
琼东南盆地中生代潜山储集空间特征照片a. Y81-b井,埋深2 909.0 m,花岗碎裂岩,风化成砂砾质,孔隙发育,单偏光;b. Y81-a井,埋深2 960.5 m,花岗闪长岩,溶蚀孔洞发育,裂缝发育,单偏光;c. Y81-a井,埋深2 982.0 m,花岗岩,多期裂缝发育,呈缝网结构,单偏光;d. L321-a井,埋深4 011.0 m,花岗岩,局部长石风化成黏土化,正交偏光;e. L321-a井,埋深4 167.0 m,二长花岗岩,碎裂结构,裂缝发育,正交偏光;f. L261-a井,埋深3 712.0 m,花岗岩,碎裂结构,裂缝发育,有溶蚀扩大,单偏光;g. Y81-a井,埋深2 960.5 m,花岗岩,风化成砂砾状,孔隙发育,壁心;h. Y81-a井,埋深3 054.1 m,二长花岗岩,相对致密,裂缝闭合,壁心;i. L321-a井,埋深4 290.1 m,二长花岗岩,裂缝发育,方解石脉体充填,壁心;j. L321-a井,埋深4 257.0 m,二长花岗岩,多期裂缝发育,呈缝网结构,壁心;k. L261-a井,埋深3 704.3 m,二长花岗岩,多期裂缝发育,呈缝网结构,壁心;l. L261-a井,埋深3 623.4 m,二长花岗岩,多期裂缝发育,呈缝网结构,发育溶蚀孔洞,壁心"
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