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u-dating AND δ^(18)O, δ^(13)C FEATuRES OF SPELEO-THEMS IN MAOMAOTOu BIG CAVE, GuILIN
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Chinese Science Bulletin 1986年 第12期31卷 835-838页
作者: 汪训一 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
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 sand... 详细信息
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