沁水
1.Simulation of History of CBM Concentration-Dissipation in Middle Southern Qinshui Basin
3.CBM development potential of high rank coal with reference to Qinshui coal field,Shanxi
4.EFFECT OF PORE STRUCTURE ON CBM TRANSPORT——TAKING QINSHUI BASIN AS THE EXAMPLE
5.Prediction of higher-permeability region for CBM exploration based on multivariate regression analysis:A case study from Qinshui Basin
6.Thermal maturation of Permo-Carboniferous coal seams were mainly controlled by geothermal anomaly of Late Mesozoic, on the basis of this geothermal anomaly, different structural units has different metamorphic rank due to plutonic metamorphism and regional magmatic metamorphism.
7.According to the aforementioned research, we could find the geological regionalization of coalbed gas reservoir formation in Qinshui Basin, which is shown that the advantaged area in the south of the Basin is Yangcheng and north Jincheng, including Panzhuang, Fanzhuang and Zhengzhuang;
8.The higher-permeability region for CBM exploration are Panzhuang-Yangcheng, Yangquan-Shouyang and Taiyuan Xishan coalfield in Qinshui Basin.
9.In Qinshui Basin, the fresh-water peat swamp facies and forest peat swamp facies were the sedimentary environments of forming good reservoirs, but the drained peat swamp fecies was difficult to form good reservoirs in general.
10.in Bohai Bay basin should pay attention to in-depth study of second ary hydrocarbon generation and migration; in South Huabei basin,Fenghe graben b asin and Bayinhaote basin should breakthrough the pass for gas prospecting.
