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《Geological Survey and Research》 2008-04
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Division of the Tectonic Sequences and Tectonic Evolution of Late Mesozoic-Cenozoic in Weatern Qinling

GUO Jin-jing,HAN Wen-feng(Tianjin Institute of Urban Construction,Tianjin 300384,China)  
Late Mesozoic-Cenozoic red bed deposit strata in the western Qinling,based upon their rock association,spatial distribution and tectonic deformation characteristics,can be divided into three tectonic sequences.They are J3-K1,K2-E and N tectonic sequence,which are corresponded to three tectonic evolution stages.J3-K1 tectonic sequence is composed of deep pink-gray conglomerates sandstones and shales with the black shale and coal bed.It is characteristed structurally by NEE trend folding and faulting,which could be related to NW-SE direction compression and crustal shortening lead by the oblique convergence between North China Block and Yangtze Block in Yanshan Movement.K2-E tectonic sequence is mainly composed of brick-red,pink conglomerate,sandstone and shale with grey or yellow-green shale or mud rocks.Its spatially extensive distribution indicated that at that time when it was formed,regional crustal extention existed.At the end of Eogene,NE-SW direction tectonic compression lead to form the NW trend fold and fault,which could be the results of the tectonic response to the India-Euasia plate collision.Neogence tectonic sequence is characteristed by horizontal occurrence,fined sedimentary rocks,in which the existence of red soil,fresh water carbonate and Happarion fossil and mainly distribution on the Planation surface shows that at the beginning of Neogence Period western Qinling had ever underwent long time planation,finally formed an extensive plantation surface.As the part of Tibet Plateau,rapid uplift of western Qinling could begin at the end of Neogence Period.
【Fund】: 国家自然科学基金资助(40642011)
【CateGory Index】: P542
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