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四川盆地雷口坡组层序岩相古地理

李凌 谭秀成 周素彦 邹春

西南石油大学学报(自然科学版)2012,Vol.34Issue(4):13-22,10.
西南石油大学学报(自然科学版)2012,Vol.34Issue(4):13-22,10.DOI:10.3863/j.issn.1674-5086.2012.04.002

四川盆地雷口坡组层序岩相古地理

Sequence Lithofacies Paleography of Leikoupo Formation, Sichuan Basin

李凌 1谭秀成 1周素彦 2邹春3

作者信息

  • 1. 西南石油大学资源与环境学院,四川成都610500
  • 2. “油气藏地质及开发工程”国家重点实验室·西南石油大学,四川成都610500
  • 3. 大港油田勘探开发研究院,天津大港300280
  • 折叠

摘要

Abstract

The inconsistence in different mining areas of the stratigraphic division schemes of Leikoupo Formation, Sichuan Basin, and the fact that on the karst zone strata sloughed off effected by Early Indosinian movement, brings about a problem of stratigraphic classification and lithofacies paleographic reconstitution. Guided by sequence stratigraphy theories and methods, this paper collates and stipulates the stratigraphic division schemes of Leikoupo Formation on the basin interior and reconstructs stratic lithofacies paleography by using quarternary bedding as constructive units. High precision lithofacies paleographic study demonstrates that Sichuan Basin of Leikoupo stage was in restricted-evaporated sea environment and that platform edge developed near Songpan-Ganzi oceanic trough in northwest Sichuan, where the grain bank of platform internal and fringe constitutes the main prospecting parts of Leikoupo Formation. The evolution of lithofacies paleography indicates that the bed form of basin transformed from dipping eastward to westward by the way of "seesaw" in the period of Leikoupo Formation deposition. Even in the early stage of sequence Ideposition, it still remained what the topographic configuration took on as in early Triassic, which was high westward and low eastward, while the eastward dipping trend disappeared gradually in sequencelll depositional period. Yet, after that period there presented a miniature of uplift-hollow framework in the sequence IV—V depositional period on the basin interior. From sequence VI on, the bed form uplift-hollow framework differentiated intensively accompany with the intensity of the tectonic compression movement, forming macro-thick gypsolyte basin, whose depocencer had an apparent westward dipping trend in the depositional period of sequence VI—X.

关键词

层序地层/岩相古地理/雷口坡组/四川盆地

Key words

sequence strata/ lithofacies paleography/ Leikoupo Formation/ Sichuan Basin

分类

能源科技

引用本文复制引用

李凌,谭秀成,周素彦,邹春..四川盆地雷口坡组层序岩相古地理[J].西南石油大学学报(自然科学版),2012,34(4):13-22,10.

基金项目

国家重点基础研究发展计划项目"973"计划(2012CB214803) (2012CB214803)

中国石油科技创新基金研究项目(2011D-5006-0105) (2011D-5006-0105)

四川省重点学科建设项目(SZD0414) (SZD0414)

西南石油大学学报(自然科学版)

OA北大核心CSCDCSTPCD

1674-5086

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