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从沉积上看,中国的地质发展史,从晚元古代以来可以中三叠世印支运动中幕划分为两个截然不同的阶段,第一阶段是以海相沉积为主的海陆交互变迁过程,第二阶段是陆盆沉积发育时期。 回溯中国最早的地壳运动是阜平运动(距今约30亿年)、五台运动(距今约24亿年)及吕梁运动(距今约18亿年)。它们导致了由泰山群、五台群、滹沱群三套变质岩系组成基底的中朝陆台的形成,而在其它广阔的地区为泛海洋分布,形成海陆对峙面貌,沉积了槽盆相的长城系—青白口系—蓟县系,并由海向陆逐渐转化。晋宁与澄江运动(约7—8亿年前)使扬子、塔里木、中朝等地台联为古中华陆。
From sedimentary perspective, the history of geologic development in China can be divided into two distinct phases since the Late Proterozoic in the middle Triassic Indo-Chinese Movement. The first phase is the process of interdependence between land and sea based on marine sedimentation The second stage is the basin sedimentary development period. Back to China’s earliest crustal movements are the Fuping Movement (about 3 billion years ago), the Five Sports (about 2.4 billion years ago), and the Luliang Movement (about 1.8 billion years ago). They resulted in the formation of the Sino-North Korea terrestrial platform formed by the three sets of metamorphic rocks of Taishan Group, Wutai Group and Hutuo Group, while in other broad areas they are distributed in a broad ocean, forming the confrontation between land and sea and sedimentary facies Great Wall Department - Qingbaikou Department - Jixian Department, and gradually transformed from the sea to land. Jinning and Chengjiang Movement (about 700 million to 800 million years ago) brought together Taiwan, the Yangzi, Tarim, and North Korea as the ancient China Land.