摘要
研究表明：印支运动的褶皱作用非常轻微，认为其导致华南地台盖层全面褶皱的观点是不恰当的。华南地台盖层全面褶皱是由晚三叠世以来多期次继承性造山运动形成的同步—类同步褶皱。主要褶皱时代很晚，在南北太平洋大地构造域是晚侏罗世至中始新世。
The recent studies show that the overall folding of the cover of South China platform can not caused by the Indosinian week folding in south China but caused by multiphase inherited orognies after late Triassic. The principal folding is quite late. In the northwest Pacific domain, the folding age is from Late Jurassic to Middle Eocene, and in the Tethys domain it is between Middle and Late Eocene.
出处
《地质与勘探》
CAS
CSCD
北大核心
1999年第4期5-7,11,共4页
Geology and Exploration
基金
广西壮族自治区自然科学基金资助项目
关键词
华南地区
地台盖层
褶皱
形成时期
地台
cover of south China platform, indosinian tectogenesis, inherited orogeny, Meso-Cenozoic
