U-DATING AND δ^(18)O, δ^(13)C FEATURES OF SPELEO-THEMS IN MAOMAOTOU BIG CAVE, GUILIN

作     者：汪训一 WANG XUNYI(Institute of Karst Geology, Ministry of Geology and Mineral Resources, Guilin)

作者机构：Institute of Karst Geology Ministry of Geology and Mineral Resources Guilinhe Maomaotou Hill (or called Guangming Hill) is located on the right shore of the Tahua River NW of Guilin and is a peak bunch formed by some cone peaks of aparry sandclastic limestones relict microcrystalline sandclastic limestones and micrite lime-stones of Rongxion Formation of the early Devonian. The area of the hill is 0.92 km~3 and its relative altitude ca. 250m. The caves discovered in the hill from south to north are the Ludi Cave the Big Cave the Feisi Cave and the Chuan Cave (Table 1) among 

出 版 物：《Chinese Science Bulletin》 (科学通报(英文版))

年 卷 期：1986年第31卷第12期

页      面：835-838页

学科分类：0709[理学-地质学] 081803[工学-地质工程] 07[理学] 08[工学] 0818[工学-地质资源与地质工程] 

主　　题：altitude north dating shore bunch Chuan GUILIN U-DATING AND seasonal abundant 

摘      要：The Maomaotou Hill (or called Guangming Hill) is located on the right shore of the Tahua River, NW of Guilin and is a peak bunch formed by some cone peaks of aparry sandclastic limestones, relict microcrystalline sandclastic limestones and micrite lime-stones of Rongxion Formation of the early Devonian. The area of the hill is 0.92 km^3 and its relative altitude ca. 250m. The caves discovered in the hill, from south to north, are the Ludi Cave, the Big Cave, the Feisi Cave and the Chuan Cave (Table 1),