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《成都地质学院学报》 1992-04
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PALEOKARST-RELATED NATURAL GAS RESERVOIRS OF MAJIAGOU FORMATION, ORDOS BASIN

Zhang Jinquan;Geng Aiqin;Chen Hongde;Zhen Rongcai;Zheng Chenguang;Zhang Jisen  
After the deposition of early Ordovicitan, Ordos Basin uplifted and suffered weathering erox-ion. Paleokarst system developed on Majiagou dolestone between 30~100m in thickness beneath theOrdovician unconformity. In different karst morphologic units, the development of solution fractures,vugs and caves, the types and distributions of karst breccias, and the karst facies associations in se-quence are quite different. The most favorable karstified morphology to form reservoirs is located inkarst slope, where the surface water leached vertitully along the fractures and underground runoffmoved horizontally near the phreatic water table. The strong aiternating circulation and dissolution ofkarst water resulted in formation of fracture-soution cavity reservoir dominating by stratified solutionvugs. Although the porosity and permeability of the reservoir is unhomogeneous and very variable, thereservoir shows the characteristics of stable regional distribution and large-scale gas production becauseof the gentle dipping occurence of Jingbian-Zhidan-Yichuan karst slope.
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