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《JOURNAL OF GUIZHOU NORMAL UNIVERSITY(NATURAL SCIENCE)》 1997-02
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KARST LANDFORM DEVELOPMENT AND SPELEOGENISIS OF THE LONGGONG AREA, GUIZHOU

He Caihua Xiong Kangning (Departement of Resource and Environment Science, Guizhou Normal University, Guiyang 550001)  
The Longgong drainage system consists of western and eastern branches connected by surface overflow or underground rivers in seasons of a year With the neotectonic uplift and river incision, the karst landforms were rejuvenated and distributed by an alternation of fenglinplain, fenglin-valley (basin) and fengcong-poljie(depression) from the north to the south Formation and development of the caves in the area are strongly related to changes of the underground river system The upper-levelled caves are characterized by through-cave with phreatic features The middle/lower-levelled caves, speleothem on the roof and riverbed on the floor, are connected with each other and developed deppdard along structural weak zone Fissured-section of the caves are visibale
【Fund】: 贵州省自然科学基金
【CateGory Index】: P931
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