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《Geological Science and Technology Information》 2001-01
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EXTRUSION TECTONICS IN OROGENIC BELT

Zeng Zuoxun 1 Yang Weiran 1 Franz Neubauer 2 Liu Lilin 1 Guo Tieying 1 ( 1.Faculty of Earth Sciences,China University of Geosciences,Wuhan Hubei China,430074; 2.Institute of Geology and Paleontology,University of Salzburg,A 5020,Salzburg,Aust  
The model of extrusion tectonics has been generalized to the research of three dimensional extrusion from two dimensional extrusion research.In the Himalaya orogenic belt,Higher Himalaya crystalline between the north dipping main central thrust fault and the north dipping Rongbushi normal fault (or Southern Tibet detachment system) yields ductile extrusion in wedge shape.The finite element modeling with large deformation in noncontinuous media has proved that the normal and thrust faults dipping in the same direction can develop contemporarily under the same contraction regime.On the basis of works of previous researchers,the authors put forward a three dimensional model of pipe shaped extrusion for the eastern Alps.The upper brittle layer is divided into three parts,namely,the left lateral strike slip belt in the north part,the right lateral strike slip belt in the south part and the middle extrusion wedge.In the process of south Alps Europe foreland collision,not only the vertical extrusion,but also the lateral extrusion develops.On the section parallel to the maximum shortening direction (MSD) the box shaped anticline uplift revolved into wedge shaped extrusion with the combination of the thrust thrust faults,forming the pipe with a triangular section.While on the section perpendicular to the MSD,the middle ductile layer flows inhomogeneously and form pipe shaped laminar flows.It is put forward that a three dimensional decollement extrusion of a composite orogenic body exists in the adjoining area of Sichuan,Gansu and Shaanxi Provinces.It consists of the Western Qinling and Eastern Songpan Garz orogenic belts and develops between the West Sichuan foreland and the rigid indenter of the Qilian North Qinling Caledonian orogenic belt.It is divided into three first order tectonic units,by the Maqu Lueyang fault trending in NNW and the Qingchuan Maoxian fault trending in NE.They are Western Qinling décollement extrusion belt,Motianling Zoig décollement extrusion wedge and Longmenshan décollement extrusion thrust belt.The wedge is further subdivided into Motianling décollement extrusion body and Zoig décollement extrusion body by the N S trending Mingjiang fault.The Motianling presents westward lateral extrusion except the inhomogeneous uplift of the different tectonic units.
【Fund】: 国家自然科学基金资助项目 !( 49772 14 7;;49972 0 6 8);; 国土资源部“九五”攻关课题! ( 95 -0 2 -0 0 2 -0 1) ;; 湖北省地球表层系
【CateGory Index】: P542
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