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《Chinese Geology》 2003-04
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Tectonic deformation and origin of tongue-like gneiss in the Jinping area, northern Jiangsu

PAN Ming-bao1,2, CHEN Huo-gen2, Xie Guo-ai1, ZHANG Qing-long1 , CHEN Shou-ju2(1. Department of Earth Science, Nanjing University, Nanjing 210093, Jiangsu, China;2. Jiangsu Institute of Geological Survey, Nanjing 210018, Jiangsu, China)  
According to detailed mapping in the Jinping area on the southern edge of the Su-Lu orogen, it is affirmed that the boundary between the ultrahigh-pressure metamorphic belt and high-pressure metamorphic belt is a ductile shear zone. No regional folds occur in the area, but instead, as the Jushan granitic gneiss and metavolcanic rocks of the Yuntai Group-complex form a competent rock layer, an incompetent rock layer was formed by metasedimentary rocks of the Jinping Group-complex; they combine to form a "layer cake"-style rock assemblage. In the Indosinian period, dextral shear gave rise to heterogeneous shear deformation; as a result, a rootless tongue-like fold of the Jushan granitic gneiss was formed. It is about 10 km long from north to south and about 5 km wide. The material movement is south-vergent in the Jinping area.
【Fund】: 江苏省国土资源厅科研项目苏鲁造山带南缘构造演化与成矿作用。
【CateGory Index】: P542.2
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