石油与天然气地质 ›› 2020, Vol. 41 ›› Issue (5): 985-995, 1047.doi: 10.11743/ogg20200509
宁超众1(), 胡素云1, 潘文庆2, 姚子修1, 李勇1, 袁文芳2
收稿日期:
2018-02-22
出版日期:
2020-10-28
发布日期:
2020-10-22
作者简介:
宁超众(1988-),男,博士、工程师,油田开发地质研究。E-mail:基金资助:
Chaozhong Ning1(), Suyun Hu1, Wenqing Pan2, Zixiu Yao1, Yong Li1, Wenfang Yuan2
Received:
2018-02-22
Online:
2020-10-28
Published:
2020-10-22
摘要:
塔里木盆地哈拉哈塘地区奥陶系良里塔格组发育典型的表生岩溶体系,形成特征性的喀斯特地貌及地下岩溶洞穴系统。首先利用地震资料表征了良里塔格组顶部喀斯特地貌,然后应用岩心、镜下及测井资料研究了地下岩溶洞穴系统的基本特征,并通过RMS振幅和方差融合技术刻画了岩溶洞穴系统的展布。结合本区地质背景,探讨了岩溶体系发育的控制因素。研究表明,良里塔格组顶部喀斯特发育岩溶高地、岩溶斜坡、岩溶槽谷和落水洞等地貌要素,不同的地貌要素具有不同的分布特征;其内部岩溶洞穴系统发生垮塌、充填及压实,岩溶洞穴通道呈直线形态并交织成复杂网状。控制该区岩溶体系发育的因素有:低水位期海平面下降、先存断裂及裂缝、地表河流体系。
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