摘要
按照板块构造理论及活动论、阶段论的思想 ,大致以中晚三叠世为界 ,将中国南方自震旦纪以来大地构造演化历史划分成海相盆地演化阶段 ( Z～ T2 )及陆相盆地演化阶段 ( T3 ～ Q)两大阶段 ;又可进一步细分为扬子克拉通及其周缘裂谷盆地 ( Z～ C-1q)、裂谷—克拉通—被动大陆边缘盆地 ( C-1c～O1)、被动陆缘—克拉通—前陆盆地 ( O2 ～ S)、加里东运动 ( S末 )、裂谷—克拉通盆地 ( D～ T1)、克拉通残留海盆 -弧后 (浊积 )盆地 ( T2 )、印支运动 ( T2 ～ T3 )、华北—华南板块焊合、古特提斯封闭与前陆盆地的形成 ( T3 ～ J2 )、压扭背景下的改造作用及拉分盆地的形成 ( J3 ～ K1)、伸展—裂陷盆地的形成 ( K2 ～ E)、喜马拉雅运动 ( E末～N初 )及披盖性构造层的形成 ( N～ Q) 1 2个阶段。特别是对南方自中晚三叠世以来的大地构造演化及其对现存油气的控制作用进行了系统研究 ,提出了晚侏罗世 -早白垩世燕山运动对南方中生界、古生界原生油气藏的保存与破坏起到了决定性作用及燕山、喜马拉雅运动控制了现今南方原生、次生及再生烃 (二次生烃 )
The tectonic evolution of southern China after Sinian was mainly related with the drifting and rift colliding history between Yangtze plate, Cathaysian plate, North China plate, Kula Pacific plate, India plate, Indosinian massif, Northern Viet Nam massif, Songpan massif, Yidun massif, Changdu Simao massif, Baoshan massif, Tengchong massif and Hainan massif, etc. According to the thoughts of plate tectonics and mobilism, the authors divide the tectonic evolution history of southern China as 2 stages, that is, the marine basin stage (Sinian to Middle Triassic) and continental basin stage (Upper Triassic to Quaternary), and further divide it into 12 sub stages, that is, the Yangtze craton & peripheral rift basin(Sinian to Lower Cambrian Qiongzhushi Stage), rift craton passive continental margin basin (Lower Cambrian Changlangpu Stage to Lower Ordovician), passive continental margin craton foreland basin(early Upper Ordovician to Silurian), Caledonian movement(the end of Silurian), rift craton basin(Devonian to Lower Triassic), craton residual marine basin & back arc turbidite basin(Middle Triassic), Indosinian movement (Middle Triassic to Upper Triassic), collision between North China plate and South China plate, close of paleo Tethys and formation of foreland basins (Upper Triassic to Middle Jurassic), transformation & formation of pull apart basins under background of compress shearing (Upper Jurassic to Lower Cretaceous), formation of continental rift basins (Upper Cretaceous to Paleogene), Himalayan movement (at the end of Paleogene to early Neogene) and formation of draping synthem(Neogene to Quaternary ). Especially, the paper makes a systematical research on the tectonic evolution after middle late Triassic and its controlling over the existent hydrocarbon in southern China, and puts forward the new viewpoints that the Yanshanian movement of late Jurassic to early Cretaceous controlled the preservation or destruction of the Mesozoic & Paleozoic primary reservoirs and the Yanshanian and Himalayan movements controlled the distribution of the existent primary, secondary and hydrocarbon regeneration (the second hydrocarbon generation) reservoirs in southern China. The tectonic evolution before the Yanshanian stage controlled the formation and distribution of the Mesozoic & Paleozoic primary reservoirs in southern China, which are chiefly distributed around paleo uplift and the intensity of Yanshanian movement in late Jurassic to early Cretaceous controlled the preservation or destruction of these primary reservoirs. In Sichuan basin, the primary reservoirs have preserved, but in other areas of southern China, they are mostly destroyed. The tectonic evolution of Himalayan finally controlled the genetic types and distribution of existent commercial reservoirs. The primary Tertiary reservoirs are distributed in Tertiary rift basins, such as northern Jiangsu, Jianghan, Baise basins etc., the secondary Mesozoic & Paleozoic reservoirs are chiefly distributed over western areas of southern China, such as Sichuan, Cuxiong basin, and the hydrocarbon regeneration Mesozoic & Paleozoic reservoirs are mainly distributed in Tertiary rift basins in the middle lower Yangtze area.
出处
《成都理工大学学报（自然科学版）》
CAS
CSCD
北大核心
2003年第2期155-168,共14页
Journal of Chengdu University of Technology: Science & Technology Edition
基金
中国石油天然气集团公司"九五"油气勘探科技工程项目 ( 970 2 0 5 )
