ON LOPINITE,A NEW TYPE OF COAL IN CHINA

To the east of Nanchang,the capital of Kiangsi Province,there cropsout a continuous belt of Permian coal series~1 trending approximately in thedirection from N.E.to S.W.Broadly speaking,this coal belt forms a synclinal     

鄂尔多斯盆地西峰油田原油地球化学特征及其成因

通过对鄂尔多斯盆地西峰油田原油进行系统地采样和高分辨率的GC-MS、IRMS分析,研究了原油的生物标志化合物和碳同位素组成特征,并且进行了油源对比,探讨了其成因。研究资料指示了所研究原油属于同一成因类型;原油有机母质为菌藻类和高等植物,特别是高等植物为原油的形成作出了贡献;原油形成于弱还原和淡水或微咸水环境;原油均为成熟原油;原油地球化学特征和上三叠统延长组长,油层组具有亲缘关系,反映了原油主要来源于长,油层组。这些研究结果为盆地的石油勘探提供了科学依据。     

西秦岭杨河-固城一带原“泥盆系“中发现早石炭世化石

西秦岭武山杨河礼县固城一带的原"泥盆纪"地层中,发现了大量属于早石炭世的牙形刺、珊瑚和有孔虫化石,为该区地层的重新划分提供了直接的证据.这对于重新认识该区乃至整个西秦岭地区石炭纪古地理格局、地质演化历史、沉积相和沉积环境等都有重要的意义.     

青藏高原北部铁路沿线移动冰丘的特征及其灾害效应

青藏高原北部常年冻土地区部分断裂破碎带发育移动冰丘。青藏铁路沿线典型移动冰丘包括不冻泉活动断裂诱发移动冰丘、乌丽活动断裂诱发86道班移动冰丘、二道沟盆南断裂破碎带桥梁施工诱发雅玛尔河移动冰丘、断裂破碎带桥基施工诱发83道班移动冰丘和乌丽盆北断裂破碎带DK1202+668大桥中部桥墩施工诱发85道班移动冰丘。移动冰丘的形成演化与活动断裂、地下水运动、气温变化存在动力学成因联系,是青藏高原北部常年冻土地区内动力与外营力相互耦合的标志和产物。移动冰丘能够穿刺公路路基、拱曲破坏涵洞结构、导致桥梁墩台破裂和输油管道拱曲变形,产生显著的灾害效应,成为高寒环境地质灾害的重要类型。采用适当的工程措施,通过疏导、排放地下泉水,能够有效地防治移动冰丘及灾害效应。     

Post-Collisional Ductile Extensional Tectonic Framework in the UHP and HP Metamorphic Belts in the Dabie-Sulu Region, China

The present-day observable tectonic framework of the ultrahigh-pressure (UHP) and high-pressure (HP) metamorphic belts in the Dabie-Sulu region was dominantly formed by an extensional process, mostly between 200 and 170 Ma, following the Triassic collision between the Sino-Korean and Yangtze cratons. The framework that controls the present spatial distribution of UHP and HP metamorphic rocks in particular displays the typical features of a Cordilleran-type metamorphic core complex, in which at least four regional-scale, shallow-dipping detachment zones are recognized. Each of these detachment zones corresponds to a pressure gap of 0.5 to 2.0 GPa. The detachment zones separate the rocks exposed in the region into several petrotectonic units with different P-T conditions. The geometry and kinematics of both the detachment zones and the petrotectonic units show that the exhumation of UHP and HP metamorphic rocks in the Dabie-Sulu region was achieved, at least in part, by non-coaxial ductile flow in the mul     

晋城煤层气藏成藏机制

通过晋城煤层气的规模开发、压裂煤层气井的解剖、井下煤层瓦斯抽放、构造地应力场研究、煤储层大裂隙系统“CT”式解剖与煤层气封闭保存条件研究, 发现3#煤储层内部存在大量煤层气包, 构造微破裂作用促使煤层气包之间广泛合并联通, 煤层气包内部储层的非均质性弱化, 渗透率增加, 煤层气包内部的游离气体比例增加, 流体压力系统边界逐渐清晰并形成煤层气藏. 揭示煤层气藏的成藏机制, 认识煤层气藏的内部细节特征, 促进了该区的煤层气开发技术进步, 提高了井下煤层瓦斯的抽放效率.      

Lithostratigraphy, Sedimentology, and Provenance of the Balfour Formation (Beaufort Group) in the Fort Beaufort–Alice Area, Eastern Cape Province, South Africa

Abstract: The Balfour Formation has a pronounced lithological variation that is characterized by alternating sandstone- and mudstone-dominated members. The sandstone-dominated Oudeberg and Barberskrans Members are composed of lithofacies that range from intraformational conglomerates to fine-grained sediments, whereas the mudstone-dominated members (Daggaboersnek, Elandsberg, and Palingkloof) are dominated by the facies Fm and Fl. Petrography, geochemistry, and a paleocurrent analysis indicated that the source rock of the Balfour Formation was to south east and the rocks had a transitional/dissected magmatic arc signature. The sandstones-rich members were deposited by seasonal and ephemeral high-energy, low-sinuous streams, and the fine-grained-rich members were formed by ephemeral meandering streams. The paleoclimates have been equated to present temperate climates; they were semiarid becoming arid towards the top of the Balfour Formation. This has been determined by reconstructing the paleolatitude of the Karoo Basin, geochemistry, paleontology, sedimentary structures, and other rock properties, like color.     

鲜水河断裂带的构造大地测量

利用短边GPS点阵、短基线标石阵和精密激光测距 ,在与鲜水河断裂带的断层破裂带垂直的剖面上和构造盆地内进行构造大地测量 ,获得了断层软弱带和断层蠕变带上的最佳形变分布。综合利用相关地学成果和理论 ,揭示了构造形变所隐含的动力学信息 ,识别了断层应变带、塑性流变带和主断面在地面的分布范围。用外围GPS远场联测成果探讨了该断裂带的驱动力机制 ,匡正了其“左旋”运动和现今活动速度的含义。最后 ,评估了该断裂的地震活动趋势     

富氏谱分析法模拟地壳垂直运动的地学依据及其策应力模型

应用地壳波浪与镶嵌构造学说对富氏谱分析法提取地壳垂直形变信息的科学性做了地质学意义上的阐释 ,并提出了根据多期形变资料提取特定波段上构造策应力的数学模型