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塔里木盆地西北缘野外溶蚀试验研究
引用本文:唐健生,夏日元,邹胜章,梁彬.塔里木盆地西北缘野外溶蚀试验研究[J].中国岩溶,2004,23(3):234-237.
作者姓名:唐健生  夏日元  邹胜章  梁彬
作者单位:中国地质科学院岩溶地质研究所,广西,桂林,541004
摘    要:塔里木盆地西北缘的天山南麓地处暖温带大陆性干旱气候区,碳酸盐岩广为出露.采用灰岩和白云岩溶蚀试片进行了野外溶蚀试验,得出灰岩和白云岩的溶蚀速度达到0.281~0.404mm/ka;镜下鉴定,观察到溶蚀形成的微溶缝和溶孔,缝宽0.05~0.2mm,孔径一般0.1~0.25mm,反映了在大陆性干旱气候条件下,降水下渗溶滤对岩溶孔缝洞的形成起到重要作用.

关 键 词:溶蚀试验  碳酸盐岩  溶蚀速度  塔里木盆地
文章编号:1001-4810(2004)03-0234-04
修稿时间:2004年3月24日

EXPERIMENTAL STUDY ON THE FIELD CORROSION ON THE NORTHWEST VERGE OF TARIM BASIN
TANG Jian-sheng,XIA Ri-yuan,ZOU Sheng-zhang and LIANG Bin.EXPERIMENTAL STUDY ON THE FIELD CORROSION ON THE NORTHWEST VERGE OF TARIM BASIN[J].Carsologica Sinica,2004,23(3):234-237.
Authors:TANG Jian-sheng  XIA Ri-yuan  ZOU Sheng-zhang and LIANG Bin
Institution:Institute of Karst Geology,CAGS,Institute of Karst Geology,CAGS,Institute of Karst Geology,CAGS and Institute of Karst Geology,CAGS
Abstract:Carbonate rocks are widespread along South piedmont of Tianshan, northwest Tarim Basin, where is dry-warm temperate continental climate. It is proved by corrosion tests in field with slice that the corrosion rate of limestone and dolomite is 0.281~0.404 mm/ka there. Observed under microscope, fissures formed by corrosion is 0.05~0.2 mm wide and pores formed in the corrosion test is 0.1~0.25 mm in diameter, which shows the important role of infiltrated rainwater on the formation of fissures and pores under continental dry climate conditions.
Keywords:Corrosion test  Carbonate rock  Corrosion rate  Tarim Basin
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