THE BASEMENT STRUCTURE OF SICHUAN BASIN AND ITS RELATIONSHIP TO THE OVERLYING SEQUENCES
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摘要: 本文探讨的基岩,是指盆地内沉积盖层的基底,它们是变质的褶皱的早期岩系,是以明显不整合界面与上覆沉积层分界的。近年来,由于地球物理勘探工作量的增大,手段的更新,四川盆地区域地震大剖面获得较好的效果,取得了大量丰富的地震反射信息。通过钻井、地面露头和区域地质资料的综合地质解释,极大地丰富了人们对四川盆地的地质结构、沉积、构造等方面的认识,也为盆地的深层研究提供了有力的证据。本文在综合五条区域地震大剖面的基础上,仅以其中最长的一条中—S—X区域剖面(见照片)为代表进行地质综合解释,并在此基础上阐述与本文有关问题。Abstract: In accordance with the parameters selected systematically from the drilling wells and the data from regional geological surveys on the border areas of Sichuan Basin, the integrated geological and geophysical interpretations for a new completed seismic profile in the basin are carried out. Thereafter, the location of the basement structure and the relationship to its overlying and underlying strata are described on the basis of the profile across the basin from Anxian to Wenshui. It concludes that the basement of the basin consists of a central ancient rigid massif and two foldbelts located at both sides of the massif with three different geological times. Based on Chinese tectonic framework, this paper completely describes the formation of the basement and the controlling factors of the basement on the deposition and tectonic development of its overlying sedimentary sequences.
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[1] 黄汲清等,中国大地构造及其演化,科学出版社,1980年. [2] 张恺等,中国大陆板块的演化与含油气盆地特点的讨论,石油勘探与开发,1981年1期. [3] 关士聪、演怀玉等,中国海陆变迁海域沉积相与油气(晚元古代-三叠纪),科学出版社,1984年. [4] 王尚文等,中国石油地质学,石油工业出版社,1983年. [5] 韩永辉等,上扬子地台基底演化探讨,石油与天然气地质,1983年第4期.
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