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 在沁水盆地，活水泥炭沼泽相以及森林泥炭沼泽相是形成有利储层的沉积环境，而干燥泥炭沼泽相一般难以形成有利的储层。
The authors research on the middle - south of qinshui basin , analyze the numerical connection of permeability and its influencing factor and construct compound factor model by mathematics geology method 在其基础上，文中以沁水盆地中南部为研究区，通过数学地质方法，分析和研究渗透率与其影响因素的数值关系，并研究和建立渗透率影响因素复合模型。
More than forty coal samples collected from thirteen coal mines in the north , central and south parts of qinshui basin were studied in detail so as to find out the main control factor affecting pore differential development of the high - rank coal reservoirs in the basin 为查明影响沁水盆地高煤级煤储层孔隙系统差异发育的主控因素，对采自该盆地北、中及南部6个市县13个矿区的40余件样品进行了详细解剖研究。
In accordance with the main contradictions between high deterioration degree of coal and low permeability of coal bed , this paper predicts high permeability region by use of new technique and methods including stress field , curvature analysis and major stress difference analysis 针对沁水盆地煤变质程度高、煤层渗透率普遍较低的主要矛盾，利用新技术、新方法，利用应力场、曲率分析方法和主应力差分析方法预测高渗区。
The geochemical characteristics of coals from liyazhuang coal mine , sihe coal mine and fucheng coal mine of qinshui basin , shanxi province , were comparatively studied , and the thermal evolution degree , the contents of soluble organic matter and the biomarker characteristics of coals were discussed 摘要对比研究了山西沁水盆地李雅庄煤矿、寺河煤矿和附城七一煤矿煤岩的地球化学特徵，讨论了煤岩的热演化程度、可溶有机质含量、生物标志化合物特徵。
Raw material : the output of hemp in yangcheng county and qinshui is 3 , 500 tons and the city government give the help in economy and policy to build the base of raw material . so it can meet the demands of the production . some few special material can be supplied from the neighboring provinces 当地所属县阳城及附近县沁水两县大麻产量为3500吨，市政府在原料基地建设方面，给予了经济支持和政策倾斜，产量可以满足生产所需，少量特殊品种的缺口可由邻县补充供应。
Aim at the present condition that the permeability of high rank coal reservoirs and its dynamic change regulation have been rarely studied , based on the modern testing technologies and actual measure data of coalbed methane ( cbm ) well with better drainage effect in qinshui basin , using the international advanced cbm well numerical simulation software ( comet2 ) , the dynamic change regulation of the permeability of high rank coal reservoirs during gas recovery has been discussed , using the gas and water recovery process in divided stage is matched 摘要针对高煤级煤储层渗透率尤其是其动态变化规律极少开展研究的现状，基于现代测试技术和沁水盆地排采效果较好的煤层气井实测排采数据，利用目前国际上较为先进的煤层气数值模拟软件comet2 ，采用分段拟合的方法对煤层气井的产气、产水过程进行历史拟合和修正，进而对高煤级煤储层渗透率在开采中的动态变化规律进行了探讨。
Considering the genetic mechanisms of abnormal pressure of coal reserveoir in process of geologic uplifting , through quantitative simulation analysis on geologic uplifting process in qinshui basin and tabamiao district , the variety of fluid physical volume of coal reservoir causing pressure variety of coalbed gas is analyzed , which reflects the dynamic evolvement process of whole reservoir pressure in the process of geologic uplifting , resulting in conclusion that means the geologic uplifting process is an important mechanism of abnormal low pressure 摘要从煤储层在构造抬升过程中异常压力的成因机理入手，通过沁水、塔巴庙地区抬升过程的定量模拟研究，分析在整个抬升过程中煤储层流体体积的变化所引起的流体压力的变化情况，从而反映储层压力在整个构造抬升过程中的动态演化过程，得出“抬升过程是异常低压形成的重要机制”的结论。
