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Volume 30 Issue 3
Sep.  2011
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CHEN Li-xin, PAN Wen-qing, LIANG Bin, LUO Ri-sheng, ZHANG Qing-yu, GAO Xiang. The distribution characteristics of the epikarst reservoir in Lunnan Ordovician buried hill[J]. CARSOLOGICA SINICA, 2011, 30(3): 327-333. doi: 10.3969/j.issn.1001-4810.2011.03.015
Citation: CHEN Li-xin, PAN Wen-qing, LIANG Bin, LUO Ri-sheng, ZHANG Qing-yu, GAO Xiang. The distribution characteristics of the epikarst reservoir in Lunnan Ordovician buried hill[J]. CARSOLOGICA SINICA, 2011, 30(3): 327-333. doi: 10.3969/j.issn.1001-4810.2011.03.015

The distribution characteristics of the epikarst reservoir in Lunnan Ordovician buried hill

doi: 10.3969/j.issn.1001-4810.2011.03.015
  • Received Date: 2011-08-04
  • Publish Date: 2011-09-25
  • Lunnan ancient buried hill is located in the central region of Lunnan low bulge of Tabei uplift, Tarim basin. Ordovician Yingshan formation and Yijianfang formation are the major karst layers. The formation condition and the time of epigenic karstification of Lunnan ancient buried hill are very similar with Guilin karst in South China. With the study on the formation and distribution characteristics of epikarst in Lunnan ancient weathering crust and its influence factors, the following is gained in this paper. Epikarst belt, characterized by well developed karst fracture-cave system with certain connectivity, is range from 0 to 40m under the ancient weathering surface, which is the karst reservoir well developed part. The karst effective reservoir space is mainly corrosion pore, small-scale cave and corrosion fissure. The development of epikarst has close relationship with paleo-topography and paleo-hydrodynamic conditions. Under the different paleo-topography and paleo-hydrodynamic conditions, the thickness and karst shape of the epikarst, as well as scale and filling characteristics of karst fracture-cave system in the epikarst are different.

     

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