Advanced Materials Research Vols. 524-527

Abstract: Airflow temperature in mine changes with periodical change of surface air temperature, but its change pattern couldn’t be expressed by quantitative calculation currently. by differential equation of round roadway and zero dimension of boundary condition, wall rock thermal field is expressed by superposition of two thermal fields; the two thermal fields is respectively effected by annual average wind temperature and air temperature fluctuation. The paper mainly analyses wind temperature fluctuation differential equation and its definite condition; and deduces the expression of temperature fluctuation amplitude and phasing degree at different point of roadway, while surface air temperature periodically fluctuating; by calculating and analyzing, we have the conclusion that amplitude of temperature fluctuation presents downtrend of negative exponent curve with roadway length increasing; phasing degree linearly lag with roadway length increasing. The research result is greatly significant for controlling thermal damage and forecasting wind temperature for seasonal hot mine.

Abstract: Shale gas is an important unconventional natural gas resource. There is probably abundant shale gas resource in the Longmaxi Formation of the lower Silurian, Sichuan Basin, West China. Longmaxi Formation is high quality source rock, its TOC(total organic carbon) up to the most vulue 6.5 percent; the Formation more than 1percent TOC is up to 105 meters. Because of high maturity, it cannot identify the kerogen type by element Carbon and Hydron ratio, rather than carbon isotopic value. The isotopic carbon values of Kerogens are more than 29.67 permillage, which showed One Type Kerogen. In the Longmaxi Formation, source rock is up to post maturity and lack of vitrinite, so vitrinite reflectance cannot measure the source maturity. It can measure bitumen reflectance, then calculate relevant vitrinite reflectance (Ro) by bitumen reflectance to identify the organic matter thermal evolution degree. The result showed the maturity degree of organic matter equal to more than 3 percent vitrinite reflectance (Ro), which showed the source rock yielded rich thermogenic gas during the geological thermal evolution. The source rock of Longmaxi Formation has some silt partly composed of quartz mineral, up to 40 percent, which is beneficial to gas reservoir. So, it has available shale gas developed elements because of rich organic matter, high thermal maturity degree, good pool. The geological analogy method is used to assess the resource potential. Sichuan Basin has drastically similar to Michigan Basin and San Juan Basin in basin type, seal conditions, reservoir states, source rock, matched condition and so on. So they are selected as standard basin. Sixteen parameters are used to appraise the shale gas pool geological conditions. Compared with Michigan Basin and San Juan Basin by analogy method, Longmaxi Formation shale gas potential is 0.06-0.36 billion cubic meter per square kilometer.

Abstract: The Zhangjiakou Formation of Late Jurassic is mainly distributed in the Chaoyang basin in Western Liaoning. Zhangjiakou volcanic cycle may be divided into three subcycles. The volcanic rocks of Zhangjiakou Formation mainly consist of rhyolites, trachyte and trachyandesites. The volcanic rocks are characterized by high SiO₂, Al₂O₃, K₂O and Na₂O, and comparatively low MgO and TiO₂ components. σ=1.76-4.34, the average value is 2.59. Chemical composition of volcanic rocks indicates that they belong to the high-K calc-alkaline magmatic serious. The volcanic rocks are obviously enriched in incompatible elements (K, Rb, Sr, Zr, Ba, Pb, Li), and depleted in compatible elements (Ti, Co, Ni, Cr, V).The volcanic rocks is rich in LREE. The spider patterns are the right-incline. There is a slight low Eu negative abnormality and low Ce negative abnormality. The geochemistry characteristic shows that volcanic rocks of Zhangjiakou volcanic cycle were formed in the transitional environment of compressional orogeny and extensional structure. They have the basic characteristics of continental intra-plate volcanic rocks. The volcanic rocks were mainly derived from the crust materials. The lithogenesis take partial melting as a major part.

Abstract: Fuxin city is a part of low mountains and hills in Liaoning western, the plain and the hill occupy respectively 1/2. Metallogenic geological conditions of gold in Fuxin regions is superior, the types of mineral deposits is diverse, and it is dominated by Antique eon tough shear zone greenstone(mylonite) and altered rock type, volcanic type take second place, potential resource is larger, is an important production base of Liaoning province even the country. Therefore researching the geological characteristics of gold deposits in Fuxin region is of great significance.

Abstract: Taking Fuyu oil layer in the southern Fuxin Uplift of Songliao Basin as an example, through study on types and distribution characteristics of found reservoirs, this article discusses hydrocarbon accumulation characteristics and its main controlling factors in lithologic reservoirs area. The results show that reservoirs types of Fuyu oil layer are mainly local structure-lithologic reservoirs in the southern Fuxin Uplift. Characteristics of hydrocarbon accumulation is tertiary structure controlling direction, single trap controlling hydrocarbon accumulation, local structure controlling boundary and monosandbody controlling layer. General direction of hydrocarbon migration is controlled by tertiary structure, and hydrocarbon accumulation is controlled single trap. Planar distribution boundary of hydrocarbon is controlled by boundary of local structure and monosandbody in single trap, and vertical distribution layer of oil/water is controlled by vertical development characteristics of monosandbody. Local structure, single distributary channel sandbody and their array mode is main controlling factors on complicated distribution of oil/water. It is supported an important realistic significance to complicated exploration and development of lithologic reservoirs.

Abstract: There are significant hiatus between Devonian Wutong and Carboniferous Huanglong formation in Xinqiao mining area of Tongling. The two formations have very different lithology, Wutong formation is mainly continental clastic sediments, while Huanglong formation is carbonate rocks. The unconformity interface between Devonian Wutong formation and Carboniferous Huanglong formation is structural weak part, favors the aggregation of ore-forming elements. Magmatism mineralization forms significant industrial value layered massive sulfide ore body and structural weak part is as a major seam position.

Abstract: This paper relies on "The base structure and guide the middle and lower Yangtze River mine - re-controlling factors of research project" in order to study the Mesozoic intrusive rocks in the characteristics of the middle and lower Yangtze River area and distribute-on of the western part of Hubei - Jiangxi and eastern Jiangsu - Anhui comparative study of eastern and western areas. On the basis of the full collection and comprehensive study of previous data, with the actual project work and research, through comprehensive research and analysis, bounded on the east and west of Jiujiang area controlled by different tectonic framework of characteristics of intrusive rock, mainly from the petrology, rock chemistry, magma sources and diagenetic characteristics such as age were compared with paper.

Abstract: The drilling mud invasion is a dynamic process varying with time and reveal the permeability or the relatively permeability of the formation saturated with fluid. The mud invasion profile denotes the water saturation change with the radial distance from the borehole wall. The logging with the shallow depth of investigation (DOI), such as density logging, neutron logging and shallow electrical logging, often detects the information of the flushed zone. We chose DOI logging to model the slope invasion profile with the hyperbolic secant function, and the calculated logging reading comparing from the real logging reading to optimize the invasion profile. The results show that the mud invasion profile and the invasion depth are strongly affected by porosity, where the invasion depth reduces with porosity adding.

Abstract: Anisotropic information of pre-stack 3D azimuth P wave from seismic data is already one of the most efficient and economic methods from reservoir fracture examination, which requires a wide azimuth for seismic data gathering. By forward simulation of the geophysical characteristics in fractured reservoirs, the relationship between azimuth distribution areas of seismic data gathering and fracture direction is studied. Narrow azimuth for seismic data gathering is also somewhat effective to describe fracture distribution characteristics. In addition, significant seismic property difference (amplitude, damping and frequency) can be made in fractured reservoirs, thus, fracture can be effectively examined by the seismic information of different offsets. All the results in the paper get excellent practical application.

Abstract: The NW Guizhou Pb-Zn metallogenic district is an important part of the Yunnan – Sichuan - Guizhou Pb-Zn metallogenic province (SYG), and also is one of the important Pb-Zn producers in China. We analyzed the Pb isotopic compositions of sulfides, hosting rocks and basement rocks, the results show that the ²⁰⁶Pb/²⁰⁴Pb, ²⁰⁷Pb/²⁰⁴Pb, and ²⁰⁸Pb/²⁰⁴Pb ratios of sulfides range from 18.029 to 19.900, 15.357 to 17.716 and 38.004 to 40.695, respectively. The ²⁰⁶Pb/²⁰⁴Pb, ²⁰⁷Pb/²⁰⁴Pb and ²⁰⁸Pb/ ²⁰⁴Pb ratios of hosting rocks and basement rocks range from 18.397 to 19.483, 15.545 to 16.700 and 38.204 to 39.140, respectively. This indicates that the compositions of Pb isotopes of sulfides are basically consistent with that of hosting rocks and basement rocks, so the metals were sourced from various strata of carbonate rocks and underlying rocks.