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《JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY》 1998-01
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PRELIMINARY DISCUSSION ON UPLIFT BEDDING DELAMINATION STRUCTURES IN FOPING AREA, QINLING

Wang Genbao (Synthetic Research Team, Shanxi Buarea of Geology and Survey, Gaoling 710204) Li Sanzhong (Northwest University, Xi’an 710069)  
Foping dome in the Qinling orogenic belt consists of basement gneiss(core), detachment fault(contact plane) and sliding sedimentary seguence(cover). It is revealed, through synthetic analysis, on rock assemblages, early kinematics, characteristics of metamorphism and deformation, and geochronological data, that the Foping dome was formed before, transformed by Hercynian and Indosinian orogenic folding, and Yanshanian thrusting and strike sliping. Foping dome, different from metamorphic core complex, underwent uplift bedding delamination structural evolution from Mesoproterozoic to Caledonian. This process is important for the development of the Qinling orogenic belt. Therefore, it suggests vertical accretion of lithosphere in deep crustal setting of orogenic belts and shows its importance in continental dynamics.
【CateGory Index】: P542.3
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