石油学报 ›› 2021, Vol. 42 ›› Issue (3): 378-398.DOI: 10.7623/syxb202103011
邵珠福1,2,3, 张文鑫1, 毛毳1, 栾锡武2, 钟建华4, John Howell3, 刘泽璇1, 赵冰1, 冉伟民2, 刘晶晶1
收稿日期:
2019-12-30
修回日期:
2020-07-21
出版日期:
2021-03-25
发布日期:
2021-04-09
通讯作者:
邵珠福,男,1984年9月生,2007年获中国石油大学(华东)学士学位,2014年获中国石油大学(华东)博士学位,现为东北石油大学地质学专业副教授,主要从事沉积学和石油地质学专业研究工作。
作者简介:
邵珠福,男,1984年9月生,2007年获中国石油大学(华东)学士学位,2014年获中国石油大学(华东)博士学位,现为东北石油大学地质学专业副教授,主要从事沉积学和石油地质学专业研究工作。Email:kangzhu09@yeah.net
基金资助:
Shao Zhufu1,2,3, Zhang Wenxin1, Mao Cui1, Luan Xiwu2, Zhong Jianhua4, John Howell3, Liu Zexuan1, Zhao Bing1, Ran Weimin2, Liu Jingjing1
Received:
2019-12-30
Revised:
2020-07-21
Online:
2021-03-25
Published:
2021-04-09
摘要: 北美加利福尼亚地区良好的露头和北海油田的成功勘探与开发为砂岩侵入体研究提供了范例。砂岩侵入体广泛发育于晚元古代-全新世的多种沉积体系中,以深水环境居多。侵入体岩性以浊积体的中砂岩-细砂岩最为常见,宿主层以泥岩、页岩为主。侵入体系统包括供源砂体、侵入(出)体、宿主层和断裂体系4个构成要素和砂岩脉、砂岩床、砂岩柱、侵出体和复合体5种类型。侵入体外部呈碟状-翼状结构、锥形结构和顶梁复合结构3种类型,侵入体顶部发育丘型变形,内部块状或类层理状,常见侵蚀边、泥岩撕裂屑和各种软变形构造,呈拼图状。侵入体形成条件包括未固结供源砂体、低渗透—非渗透覆盖层、孔隙流体超压和砂体优势通道4部分,地震液化、差异压实、沉积负载、区域构造应力、流体流动是最常见的触发机制。侵入体形成过程包括孔隙流体超压、供源砂体液化、水力压裂与流化、砂体充注和砂体再沉积5个过程。侵入体增加了储层体积,沟通了砂体,可形成侵入型圈闭,还可用于恢复区域古应力场,但也可能导致盖层封闭性破坏和水窜。侵入时间确定、侵入后地质过程以及触发机制确定性等研究面临挑战,多学科交叉、虚拟露头、物理模拟及数值模拟技术将是砂岩侵入体研究未来的发展方向。
中图分类号:
邵珠福, 张文鑫, 毛毳, 栾锡武, 钟建华, John Howell, 刘泽璇, 赵冰, 冉伟民, 刘晶晶. 砂岩侵入体及其油气地质意义[J]. 石油学报, 2021, 42(3): 378-398.
Shao Zhufu, Zhang Wenxin, Mao Cui, Luan Xiwu, Zhong Jianhua, John Howell, Liu Zexuan, Zhao Bing, Ran Weimin, Liu Jingjing. Sand injectites and its petroleum geological significances[J]. Acta Petrolei Sinica, 2021, 42(3): 378-398.
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