天然气地球科学 ›› 2022, Vol. 33 ›› Issue (3): 381395.doi: 10.11764/j.issn.1672-1926.2021.08.010
刘嘉伟1(),赵虎1,2(),王轶3,张文锦1,陈康4,邸志欣5
Jiawei LIU1(),Hu ZHAO1,2(),Yi WANG3,Wenjin ZHANG1,Kang CHEN4,Zhixin DI5
摘要:
四川盆地二叠系火山岩具有良好的勘探前景,而盆地东部地区多口钻井显示钻遇火山岩,但都没有展开相应的研究。基于测录井及地震等资料分析,对四川盆地东部龙会场-龙门地区二叠系火山岩识别模式及分布特征进行综合研究。结果表明:在地震剖面上,当龙潭组内部多形成一个波峰反射时,代表着火山岩发育;区内火山岩以溢流相玄武岩为主,少见凝灰岩;垂向上可划分为2个喷发期次,主要发育在龙潭组中下部;平面上火山岩分布受古地貌和基底断裂共同控制,在古地貌低洼处和基底断裂附近是火山岩主要堆积部位,厚度较大。
中图分类号:
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