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《Geology of Chemical Minerals》 1996-01
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Hong Zuoming (Regional Geological Surveying Team,Liaoning Bureau of Geology and Mineral Resources)  
In the time span between late Early Cambrian and Ordovician,the northern margin of North China plafform was covered with an epicontinental sea,the Mongolia-Helongjiang-Jilin ocean,where ocean basalts and island arc volcanic rocks were accumulated.Entering the period of Silurian to Devonian,the ocean developed a set of flysch sediments which,featuring an eugeocline,more vigorously subducted toward the platform until it was uplifted to suffer from intensive denudation with no depositions the same period.The Carboniferous-Permian times waw the ocean progressively changing into a miogeocline while the plaform itself experienced uplifting and rifting in a northeast direction.By the Triassic period,the megabasin began closing up in the presence of Indosinian movement and at the same time,the Palacozoic cover on the platform was folded to dome,together with the former,inot what is called Asian platform.
【CateGory Index】: P534.4
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