引用本文:李凤杰, 郑荣才, 周小进, 赵俊兴, 蒋斌.中国南方晚古生代构造演化与盆地原型[J].沉积与特提斯地质,2009,(2):93-99.[点击复制]
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中国南方晚古生代构造演化与盆地原型
李凤杰,郑荣才,周小进,赵俊兴,蒋斌
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(1. 成都理工大学"油气藏地质及开发工程"国家重点实验室;
2. 成都理工大学沉积地质研究院;
3. 中国石化石油勘探开发研究院无锡石油地质研究所)
摘要:
晚古生代-中三叠世,中国南方在陆块间离散-聚合的不同构造运动体制下,分别在扬子陆块内部和边缘形成了不同的盆地原型及其演化序列。在扬子陆块的西南缘,主要形成裂谷-被动大陆边缘坳陷-弧后盆地的原型演化序列;扬子陆块南缘发育裂谷到台内坳陷再到裂谷原型演化序列;扬子陆块内部主要形成台内拗陷-裂谷的原型演化序列。古特提斯洋演化对晚古生代构造和盆地原型的演化起决定性作用。
关键词:  晚古生代  中国南方  陆块离散-聚合  盆地原型
DOI:
附件
基金项目:酒泉盆地青西凹陷下白垩统湖相“白烟型”热水沉积岩研究(40672073);中国石油化工股份有限公司南方勘探开发分公司科技项目(2004-13)
Late Palaeozoic tectonic evolution and basin prototype in southern China
LI Feng-jie, ZHENG Rong-cai, ZHOU Xiao-jin, ZHAO Jun-xing, JIANG Bin
(1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, Sichuan, China;
2. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China;
3. Institute of Petroleum Geology, SINOPEC, Wuxi 214151, Jiangsu, China)
Abstract:
The distinct basin prototypes and their evolutionary sequences were developed within or along the Yangtze landmass in the divergence-convergence tectonic regimes in southern China during the Late Palaeozoic to the Middle Triassic.The rift-passive continental marginal depression-backarc basin sequences occurred along the southwestern margin of the Yangtze landmass.The rift-intraplatform depression-rift sequences were developed along the southern margin of the landmass.The intraplatform depression-rift sequences were organized within the Yangtze landmass.The evolution of the Palaeo-Tethys may have exerted an important influence on the formation and evolution of the Late Palaeozoic tectonics and basin prototypes.
Key words:  Late Palaeozoic  southern China  divergence-convergence  basin prototypes

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