成都理工大学学报（自然科学版）Issue(6)：703-712,10.DOI:10.3969/j.issn.1671-9727.2014.06.05
川中古隆起构造演化特征及其与早寒武世绵阳－长宁拉张槽的关系
Evolution characteristics of Central Sichuan palaeouplift and its relationship with Early Cambrian Mianyang-Changning intracratonic sag
摘要
Abstract
In the light of the findings of the early Cambrian Mianyang-Changning intracratonic sag, this paper makes a study related to the structure and evolution for further knowing the basic geology in Sichuan Basin.Based on the palaeotectonic reconstruction of the top of the Sinian strata and by comparing the ranges of the intracratonic sag and the paleouplift at various stages,the present paper deciphers the relationship between the Mianyang-Changning intracratonic sag and the Central Sichuan paleouplift.The result shows that Sichuan Basin can be classified into 12 areas based on the evolutionary characteristics of the intracratonic sag and the paleouplift.The paper proposes that the Central Sichuan paleouplift formed with the evolution of the Cambrian intracratonic sag.The east side and west side of the intracratonic sag are independent tectonic regions,and only during Late Triassic period,they jointed a paleouplift.Their present structural features are the Southwest Sichuan uplift and the Central Sichuan uplift,respectively,especially resulting from the differential evolutions after the Himalayan period.Therefore,the Mianyang-Changning intracratonic sag controls the primary oil and gas geological conditions and the Central Sichuan paleouplift controls the formation,adjustment and preservation of the oil and gas reservoirs of the Lower Paleozoic-Sinian strata.关键词
四川盆地/川中古隆起/拉张槽/下古生界-震旦系/烃源岩Key words
Sichuan Basin/Central Sichuan paleouplift/intracratonic sag/Lower Paleozoic-Sinian/hydrocarbon source rock分类
能源科技引用本文复制引用
钟勇,李小娟,蒋波,李亚林,张晓斌,刘树根,巫芙蓉,刘定锦,邓小江,陈胜,杨飞..川中古隆起构造演化特征及其与早寒武世绵阳－长宁拉张槽的关系[J].成都理工大学学报（自然科学版）,2014,(6):703-712,10.基金项目
国家科技重大专项（2011ZX05018-003）；国家重点基础研究发展计划“973”项目（2012CB214805）；中国石油集团山地物探试验基地项目 （）
