四川盆地中三叠统角砾岩形成机制及意义

2014年 21卷 第01期
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Genetic mechanism and geological significance of Middle Triassic breccia in Sichuan Basin


胡琳 彭博 刘显凡 王多义 廖太平 王国昌
成都理工大学地球科学学院,四川 成都 610059 成都理工大学油气藏地质及开发工程国家重点实验室,四川 成都 610059 南京大学内生金属矿床成矿机制研究国家重点实验室,江苏 南京210093 重庆科技学院石油与天然气工程学院,重庆 400042 中国石化中原油田分公司普光气田采气厂,四川 达州 636150
摘要
应用沉积学、岩石学、岩相学原理,对四川盆地中三叠统野外剖面、钻井、录井样品进行描述及镜下观察,精细辨识了中三叠统地层不同角砾岩的岩石学特征,并绘制了沉积相与角砾岩关系图、古构造与角砾岩关系图。利用岩石学统计方法分析了不同角砾岩孔隙空间特征,总结得出四川盆地内中三叠统地层主要存在3类角砾岩,即台缘斜坡角砾、膏溶角砾和洞穴垮塌角砾,其分布分别受川西台缘相带、印支运动早幕活动、川北及川南古隆起因素控制,成岩后期改造对孔隙空间的影响较大,四川盆地中三叠统洞穴垮塌角砾的孔隙空间相对较发育。
Abstract
Applying sedimentology, lithology and petrography, the outcrops, core and cuttings are observed and described. All kinds of Middle Triassic Series breccias in Sichuan Basin are identified. Then the relationship maps of sedimentary facies and breccia, and paleostructure and breccia are drawn. Based on petrology statistic method, this paper analyzes the pore characteristics of different breccias. It is concluded that there are three kinds of breccias in Middle Triassic Series of Sichuan Basin: platform margin slope breccia, gypse breccia and cave collapse breccia, which are mainly controlled by western Sichuan Basin platform margin, early Indosinian movement and northern and southern Sichuan Basin uplifts. The transformation in diagenetic stage has great influence on the pore space. The pore spaces of cave collapse breccia in Middle Triassic Series of Sichuan Basin are relatively well developed.
关键词:
角砾岩; 形成机制; 中三叠统; 四川盆地;
Keywords:
breccia; genetic mechanism; Middle Triassic Series; Sichuan Basin;
基金项目
DOI
10.6056/dkyqt201401003