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Volume 34 Issue 2
Apr.  2015
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Article Navigation >  CARSOLOGICA SINICA  > 2015  >  34(2): 126-135
DAN Yong, LIANG Bin, CAO Jian-wen, ZHANG Qing-yu, HAO Yan-zhen, LI Jing-rui. Eogenetic karstification in carbonatite and its significance for hydrocarbon geology[J]. CARSOLOGICA SINICA, 2015, 34(2): 126-135. doi: 10.11932/karst20150205
Citation: DAN Yong, LIANG Bin, CAO Jian-wen, ZHANG Qing-yu, HAO Yan-zhen, LI Jing-rui. Eogenetic karstification in carbonatite and its significance for hydrocarbon geology[J]. CARSOLOGICA SINICA, 2015, 34(2): 126-135. doi: 10.11932/karst20150205
shu

Eogenetic karstification in carbonatite and its significance for hydrocarbon geology

doi: 10.11932/karst20150205
  • 1.

    Institute of Karst Geology, CAGS / Key Laboratory of Karst Dynamics,MLR&GZAR/Institute of Sedimentary Geology, Chengdu University of Technology

  • 2.

    Institute of Karst Geology, CAGS / Key Laboratory of Karst Dynamics,MLR&GZAR

  • Publish Date: 2015-04-25
    Abstract
  • Solution caves or big karst caves can be generated in carbonatite by eogenetic karstification, which is very important for the study of distribution and genesis of such caves in karst areas of the Tarim and Sichuan basins. However, young carbonate karst is few in amount and poorly studied in China. So, a large number of foreign literature about this issue were collected and reviewed in this paper. The purpose is to present features of the caves by eogenetic karst and their corrosion mechanism, and the petroleum geological significance. (1) Young carbonatite is characterized poor cementation, loose structure, and high porosity and permeability, with uniform medium space. (2) Eogenetic karst is obviously associated with rise and fall of sea level. Especially in islands or coastal areas with fresh-salt water interaction zones, the karstification featured by mixed water is relatively intense. (3) Holes or caves which formed by eogenetic karst have such patterns that flank margin caves develop in islands while channels of mixed zones appear in coastal karst. (4) Development of karst caves depends on the CO2 content of the freshwater, hydrological power of the mixed transition zone, and the change rate of sea level. (5) Eogenetic karst provides a theoretical reference for studying the short-term exposure of karstification during geological times. Such research will help understand formation mechanisms of hole-cave type carbonate reservoirs in internal karst areas and guide the distribution prediction of hole-cave type reservoirs in carbonatite regions.

     

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