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A PRELIMINARY RESEARCH ON CONTEMPORA-NEOUS SLUMP BRECCIA AT THE FRONT OF XUJIASHAN-JINGZISHAN THRUST ON NANJING-ZHENJIANG MOUNTAIN RANGE

Zhang Yongkang, Zhang Jian, Ju Jijing (Jiangsu Regional Geological Party)  
The present paper suggests, a special kind of breccias found in the front margin of Xujiashan-Jingzishan thrust fracture on Nanjing-Zhenjiang mountain range should be considered as contemporaneous slump breccia formed on the advancing process of the thrust fracture , replacing the original conception that they were gypsumgenic breccia or karst cave accumulates or basal conglmerate rocks of Huangmaqing Formation. It is revealed by study that this set of breccias on the process of overthrusting of the Xujiashan-Jingzishan fracture was a drop terrene or incongruent slump body when the upper side of the nappe advanced northward to sedimentary basin, and on the other hand was tectonic-sedimentary breccias when the upside nappe margin folded, the front rim downcasted and the topography disequilibrated that resulted in an accumulative environment of piedmont and downcast slumping breccia. This kind of breccias is an important evidence that proved the cxistance of low-angle thrust fracture.
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1 Zhang Yongkang,Zhang Jian,Ju Jijing (Jiangsu Regional Geological Party);A PRELIMINARY RESEARCH ON CONTEMPORANEOUS SLUMP BRECCIA AT THE FRONT OF XUJIASHAN-JINGZISHAN THRUST ON NANJING-ZHENJIANG MOUNTAIN RANGE[A];[C];1985
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