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《Acta Sedimentologica Sinica》 2004-01
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Late Neoproterozoic Sedimentations of the Carbonate-Detrital Flows in Longshou Mountains, Northwest China:Implications for Its Tectonic Environments

LI Wen yuan 1,2 YANG Peng fei 2 1(Xi'an Institute of Geology and Mineral Resources, Xi'an 710054) 2(Northwest University,Xi'an 710069)  
In Longshou Mountains of the southwestern margins of North China's Plate, there is extensively a series of Pre Cambrian sedimentary of the detrital flows consisting of dominant carbonate, and the sedimentary rocks have also been found in recent years. The rocks are characterized by chaotic gravels on grain sizes, dominant dolomite gravels, bed rounded gravels showing angulate subangulate, and textures of matrix support. In the region the sediments distributed continuously, but its thickness is various from several meters to tens of meters, locally transforming to volcanic rocks. On the basis of the isotopic ages and micro paleobotanic fossils of the over and underlain strata, the sedimentary rocks were suggested forming in late Neoproterozoic era. Its origin is thought to be the sediments of the carbonate -fragmental flows, on a sedimentary-tectonic environment of paleo-continental rift, coming from large quantities of collapse files on slope of continental rift due to crustal movement rapidly to lead to breakdown of sedimentary rocks on steady platform. So these rocks are the typical sediments of the continental rift, and important significance on implication for the tectonic environments. In Longshou Mountains and neighboring area the distribution of large quantities of the late Neoprozoic sediments of palaeo-fargmental flows indicate that in that time a large scale of continental rift had occurred and consistent with splitting recognition of the Rodinia continent globally.
【Fund】: 中国地质调查局地质调查项目资助
【CateGory Index】: P512.2
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