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川中—川西北加里东期古隆起对比研究

陈涛 李智武 李金玺 童馗 王自剑 蔡鸿燕 袁梦雨

沉积与特提斯地质2023,Vol.43Issue(4):675-687,13.
沉积与特提斯地质2023,Vol.43Issue(4):675-687,13.DOI:10.19826/j.cnki.1009-3850.2022.03007

川中—川西北加里东期古隆起对比研究

A comparative study of the central Sichuan paleo-uplift and the northwest Sichuan paleo-uplift during Caledonian period

陈涛 1李智武 1李金玺 2童馗 3王自剑 3蔡鸿燕 3袁梦雨3

作者信息

  • 1. 成都理工大学沉积地质研究院,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
  • 2. 成都理工大学地球物理学院地球勘探与信息技术教育部重点实验室,四川 成都 610059
  • 3. 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
  • 折叠

摘要

Abstract

The Caledonian paleo-uplifts in the Sichuan Basin are mainly located in the mid-west and northwest parts of the basin.Reconstructing and analyzing the formation and evolution of the Caledonian Middle Sichuan paleo-uplift and the northwest Sichuan paleo-uplift can provide new insights and perspectives for the future oil and gas exploration in the Sichuan Basin.Based on the results of the published borehole and seismic data,this study has carried out comparative analyses of the stratigraphic features between the middle and northwest parts of the Sichuan basin,and then identified the distribution of the pinching point,unconformity truncation point,and onlap point for each layer of the Caledonian paleo-uplift in the Sichuan Basin.On this basis,using seismic profiles and cross well lines,we have detailedly depicted and reconstructed the formation and tectonic evolution process of Caledonian paleo-uplifts in the Sichuan Basin.The evidence shows that the Caledonian paleo-uplifts were initially formed from the Late Ordovician to the Early Silurian,and they were slightly readjusted during the Late Silurian Hanjiadian period.The paleo-uplifts reached their maximum distribution range in the Early Silurian and finalized before Permian.The Duyun Movement and the Yunan Movement in the region were key tectonic movements affecting the formation of Caledonian paleo-uplifts in the Sichuan Basin.It is concluded that the Caledonian paleo-uplifts in the Sichuan Basin mainly experienced four stages of tectonic evolution:the differential uplift-fall stage(Z—∈1m),the developmental stage(∈1q—S 1),the denudation and flattening stage(S2—C),and the stable burial stage(P—T2).

关键词

四川盆地/加里东古隆起/地震解释/形成演化/关联性

Key words

Sichuan Basin/Caledonian paleo-uplift/seismic interpretation/formation and evolution/relevance

分类

天文与地球科学

引用本文复制引用

陈涛,李智武,李金玺,童馗,王自剑,蔡鸿燕,袁梦雨..川中—川西北加里东期古隆起对比研究[J].沉积与特提斯地质,2023,43(4):675-687,13.

基金项目

国家科技重大专项(2017ZX05005003-007) (2017ZX05005003-007)

沉积与特提斯地质

OA北大核心CSCDCSTPCD

1009-3850

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