石油与天然气地质 ›› 2023, Vol. 44 ›› Issue (5): 1243-1255.doi: 10.11743/ogg20230513
李涵1,2,3(), 付金华2,3, 季汉成1(), 张雷2,3, 佘钰蔚2,3, 官伟4, 井向辉2,3, 王红伟2,3, 曹茜2,3, 刘刚2,3, 魏嘉怡2,3
收稿日期:
2023-05-02
修回日期:
2023-08-20
出版日期:
2023-10-19
发布日期:
2023-10-19
通讯作者:
季汉成
E-mail:lihan1_cq@petrochina.com.cn;jhch@cup.edu.cn
第一作者简介:
李涵(1993—),女,博士研究生,石油天然气地质。E-mail:基金项目:
Han LI1,2,3(), Jinhua FU2,3, Hancheng JI1(), Lei ZHANG2,3, Yuwei SHE2,3, Wei GUAN4, Xianghui JING2,3, Hongwei WANG2,3, qian CAO2,3, Gang LIU2,3, Jiayi WEI2,3
Received:
2023-05-02
Revised:
2023-08-20
Online:
2023-10-19
Published:
2023-10-19
Contact:
Hancheng JI
E-mail:lihan1_cq@petrochina.com.cn;jhch@cup.edu.cn
摘要:
鄂尔多斯盆地西南部陇东探区上古生界二叠系太原组铝土岩系天然气勘探近期取得重大突破,开辟了新的勘探领域。但是目前对于铝土岩系分布及储层发育特征认识不清,制约了勘探进程。基于岩心观察、薄片、测录井及地震等资料,通过分析铝土岩系的物源、沉积环境及形成过程并探讨铝土岩系储层特征及形成机理,建立了铝土岩系形成分布模式及储层发育模式。研究认为:①陇东地区铝土岩系物源主要来自下古生界马家沟组碳酸盐岩。②铝土岩系发育在海退背景下温热多雨的沉积环境,垂向结构包括漏斗状、透镜状及似层状3种岩性组合类型,不同成因组合类型受岩溶的容积空间和淋滤程度等因素影响。平面上分布受古地貌控制,高地岩溶潜坑区发育漏斗状铝土岩系,垂向厚度大。斜坡区岩溶阶地以连续透镜状铝土岩为主,且横向分布具有一定范围。洼地区发育似层状铝土岩系。③岩溶负地形是控制铝土岩系发育的重要因素,泄水通道的存在是控制优势储层发育的关键因素。高地潜坑和斜坡阶地微古地貌单元是理想的铝土岩系优势储层发育区。该研究成果可为盆地内寻找铝土岩系优质储层提供依据,对新类型天然气勘探提供借鉴。
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