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华南地区加里东期造山运动,多认为发生于志留纪末。通过粤中及其邻区构造发展史的长期研究,我们认为其时空分布可分为三幕:第一幕发生于晚奥陶世末,称为台开运动,涉及闽粤大部分地区和赣中南、湘东南及桂东北地区,是广泛而强烈的一次运动。第二幕发生于中志留世末,称崇义运动,涉及湘中南、赣西和桂东北等地。第三幕发生于晚志留世末,称广西运动,涉及桂东南以外的广西境内。这三次运动在空间上形成了不同时期的造山带。第一幕至第三幕造山带呈由南东向北西、再转向南西的迁移规律。
Caledonian orogeny in southern China, and many think that occurred at the end of Silurian. Through the long-term study on the tectonic history of the development of the Central China and neighboring regions, we believe that its temporal and spatial distribution can be divided into three stages: the first stage occurred at the end of the Late Ordovician period and was called the “Taiwan-Taiwan Movement”, involving most parts of Fujian and Guangdong Provinces and Jiangxi Central South, Southeast Hunan and Northeast Guangxi, is a broad and intense exercise. Act II occurred at the end of the relics of Middle Chi, called Chongyi Movement, involving Central Hunan, Jiangxi and Guangxi Northeast China. Act III occurred Late Late Remains, referred to as the Guangxi movement, involving the territory of Guangxi outside of southeastern Guangxi. These three movements spatially formed different stages of the orogenic belt. The orogenic belts from the first act to the third act are migrated from south to east to north and then to southwest.