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我门的研究表明华北和华南地块有着复杂的地质历史.寒武纪时,这两个地块似乎均是冈瓦纳大陆的一部分,但它们是相互分离的,华南地块位于古赤道上,靠近澳大利亚的北部,而华北地块位于南纬35°.靠近伊朗、西藏和印度北部.在晚奥(?)世到石炭纪期间,冈瓦纳大陆穿过南极,发生古纬度带的倒转.然后,华北地块带着华南地块一起向北漂移.在晚石炭世和早二叠世,华北地块到达古赤道附近.二叠纪时,华北地块位于古地中海中,与伊朗、土耳其和阿拉伯毗邻.泥盆纪时,华南地块已与澳大利亚分离开,并向华北地块漂移.在晚石炭世和早二叠世,华北地块和华南地块以及印度支那地块位于古地中海中,晚二叠世,华北地块开始向北漂移,沿中亚褶皱带与西伯利亚地块碰撞.然而,直到中侏罗世,华北和华南地块才焊接在一起.自新生代开始以来,当印度板块向北漂移并与欧亚板块碰撞时,中国地块被进一步向东推挤.特别是华南地块相对于欧亚北部已向东漂移.
Our study shows that the North China and South China blocks have a complex geologic history that seems to be part of the Gondwanaland during the Cambrian, but they are separated from each other and the South China block is located on the ancient equator, Northern Australia, while the North China block is located at latitude 35 °, near Iran, Tibet and northern India. During the late Otto-Carboniferous period, the Gondwana continent crossed the Antarctic and an inversion of paleo- latitude bands occurred. North China massif drifted northward along with the South China massif. In the Late Carboniferous and Early Permian, the massifs in North China reached the vicinity of the ancient equator. During the Permian, the North China massif was located in the ancient Mediterranean Sea, with Iran, Turkey and Arabian Adjacent to the Devonian, the South China block has separated from Australia and drifted to the North China block.In the Late Carboniferous and Early Permian, the North China block and the South China block and the Indochina block are located in the ancient Mediterranean Late Permian and North China began to drift to the north and collided with the Siberia block along the Central Asian fold belt, however, until mid-Jurassic, the North China and South China blocks were welded together. Since the Cenozoic, Indian plate drifts north and plate with Eurasia At the time of the collision, the massif in China was further pushed eastwards, especially the southern China massif that drifted eastward relative to the northern Eurasian region.