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    Volume 32 Issue 1
    Jan.  2007
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    Article Contents
    FU Guang, LÜ Yan-fang, YU Dan, 2007. Major Factors Controlling Formation of Large and Intermediate Gas Fields with High Gas Accumulation Efficiency in Different Types of Basins in China. Earth Science, 32(1): 82-88.
    Citation: FU Guang, LÜ Yan-fang, YU Dan, 2007. Major Factors Controlling Formation of Large and Intermediate Gas Fields with High Gas Accumulation Efficiency in Different Types of Basins in China. Earth Science, 32(1): 82-88.

    Major Factors Controlling Formation of Large and Intermediate Gas Fields with High Gas Accumulation Efficiency in Different Types of Basins in China

    • Received Date: 2006-04-05
    • Publish Date: 2007-01-25
    • In this paper, gas accumulation efficiency was defined and calculated in terms of gas reserves, gas-bearing areas and accumulation periods. The calculation of gas accumulation efficiencies for about 60 large and intermediate gas fields in China concludes three types of large and intermediate gas fields with high, middle and low gas accumulation efficiencies. The comprehensive study of gas accumulation efficiency and different pooling conditions reveals that the formation of large and intermediate gas fields with high gas accumulation efficiency in different types of basins in China was controlled by gas supply of source rocks, gas transportation and gas seal and preservation. The creation of high gas accumulation intensity of source rocks in the large and intermediate gas fields is indispensable to the foreland basin often greater than 80×108 m3/km2·Ma, to the cratonic basin often greater than 26×108 m3/km2·Ma, and to the rift basin often greater than 60×108 m3/km2·Ma. The gas transportation velocity of transporting layer in the foreland and rift basins should often be greater than 5×10-14 m/Pa·s, that in the cratonic basin greater than 6×10-12 m/Pa·s. The comprehensive caprock seal index in the foreland basin should often be greater than 1×1010 m/s, that in the cratonic basin greater than 5×109 m/s, and that in the rift basin greater than 3×1010 m/s. The gas accumulation period in the foreland basin should often be later than the Middle Eogene, and that in the cratonic and rift basins later than the Early Eogene.

       

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