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Tianjingshi Overlapped Folding Layer Structure

ln the area of Tianjingshi(mirror stone) and Xiaoqiwa,where Middle-Late Proterozoic low-grade metamorphic rock formation distributed are often ....

Beifengkou Decollement Fault

Beifangkou bedding slip fault is a normal fault which occurs along between sandstone of Nanhua period and underlying epimetamorp-hic rocks of ....

Fault Cliff of Ercengya

The fault cliff refers to a steep cliff which formed along fault surface.The Ercengya Cliff was originally a contact zone of the mainfold fault ....

Overhanging Rock at Longmenchong

Composed of silicified sandstone,the Longmenchong overhanging fault cIiff, oriented in NNE-SSW direction, a high angle normal fault on the rim of ....

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