Remote Sensing Geological Exploration Model for Copper and Gold Deposits in the East Tianshan, Xinjiang

Based on the identification and enhancive processing of information about strata, structure, magmatite, and alteration in ore-concentrated area in the eastern Tianshan, an exploration mode of remote sensing geology is established. The mode covers basic images composed of TM (7, 4, 1), Munsell space transformation for recognizing rock type, directional matched filtering for enhancing structures, multi-layer separating and extracting weak alteration information. It will provide a rapid and effective method for geological mapping and metallogenic prediction in this region.     

Metallogenic Systems on the Paleocontinental Margin of the North China Craton

The North China Craton (NCC) is one of the largest blocks composing the continent. Different types of continental margins well developed around the NCC, along with lots of metallogenic systems of different metals and different times. Based on the study on the structural evolution of the NCC, the authors made a new division of tectonic units of the NCC. Through an analysis of the data of 1:25000 geochemical survey on stream sediments, regional geochemical features of main ore-forming elements including Au, Ag, Cu, Pb, Zn, W, Ni, Co and Mo of the NCC are discussed in the paper. Then different metallogenic systems and their forming processes and geodynamics are discussed in detail. At last, temporal and spatial distribution regularities are summarized and ten favorable ore-control factors on the paleocontinental margins are put forward, including (1) abundance of ore sources; (2) rendezvous of ore-forming fluids; (3) high thermo-dynamic anomaly; (4) remarkable Earth crust-mantle interaction; (5) cluster of     

充液井孔中的相控线阵声波辐射器在地层中产生的声场

应用有限元法研究了充液井孔中的相控线阵声波辐射器在井外地层中产生的声场,探讨了增强声源向地层的某一特定方向辐射的声波能量的方法. 采用相控线阵声波辐射器并调节其参数可以控制由充液井孔向地层中辐射的声波能量的方向,使声源向地层中的某个特定方向辐射的纵波能量得到明显提高. 在井间地震勘探和反射声波成像测井等领域中应用相控线阵声波辐射器,将有利于增大探测深度、提高探测分辨率和接收信号的信噪比.     

COMMENT ON “WHO WILL FEED CHINA”

I.MR.BROWN'SMAINOPINIONMr.LesterBrown,'presidentoftheWorldWatchinstituteintheU.S.A,publishedalongicicletitledas"WhowillfeedChina"in1994(Brown,1995),whicharousedgreatresponSeSfromhomeandabroadandattractedmuchattentionfromallsides.Theadnideasofthearticleincludethefollowingthreepoints:(1)ItisestimatedthatthepopulationofChinawillincrare490whitionfrom1990tO2030,uptol,600whition;thecultivatedlandofChinaisaffectedbythemedeAnzationoftheeconomy,andisevendisap~ng;inaddition,thepotentiality…     

三江并流带丹霞地貌景观地质成景作用

本分析对比了三江并流带黎明、罗古箐、石宝山三个丹霞地貌发育地区的景观特征,从地质学与岩石学的角度分析典型丹霞地貌景观的成景地质条件,探讨景观的地质成景作用,总结景观的成景过程。研究认为,三江并流带丹霞地貌具有自身独特的特征,岩性和构造差异是不同丹霞地貌景观差异形成的根本原因;峰林景观差异因岩层厚度、节理发育程度、交错层理不同而不同;丹霞峰林或赤壁上的“变色瀑布”是裂面或层面之间岩层水渗出沿壁下淌的结果;龟裂纹景观形成严格受岩性和节理构造控制,其发育经过了成景初期、成景中期、成景晚期三个阶段。     

古新世特提斯北缘前黑海地区盆地的演化与油气远景

此文为研究特提斯北缘前黑海地区盆地地质发展史的成果。结论是：携带有北方大陆碎屑物质的河流是其沉积作用中的主要因素。油气远景与古河流扇影响的地带有关，在那些地带出现碎屑储层的斜坡沉积。这已为古顿河—库班河和古多脑河—第聂伯尔河先三角洲的大量野外发现所证实。     

厦门市土地利用/覆盖动态变化的遥感检测与分析

在分析1990年和1997年两个时相陆地卫星TM遥感图像的基础上，得到了厦门市土地利用/覆盖的动态变化信息，并对其数量变化和空间特征进行了分析。结果表明：1990～1997年，厦门市的城镇建设用地和开发用地显著增加，耕地被占用的现象比较突出，开发用地的重点也由厦门经济特区向近郊区转移。     

Depth Distribution of Aftershocks in the China Mainland and Its Rheological Mechanism

The relationship between aftershock depths and surface heat flow in the source areas of five great earthquakes(M≥7.0)in the China mainland has been studied in this paper.The result shows that the higher the surface heat flow,the shallower is the aftershock depth,and that the distribution of aftershock depths is controlled by the rheological mechanism of brittle-ductile transition of rocks in the crust.     

Probability forecast of earthquake magnitude in Chinese mainland before A．D． 2005

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The Vertical Deformation and Horizontal Displacement Fields,Movement, and Seismicity of the Island Arc Tectonics

In this work,the vertical deformation,horizontal displacement,and stress fields of arcuate tectonics are theoretically derived from the horizontal tectonic stress; then the characteristics of tectonic movement,seismicity,and focal mechanism of arcuate tectonics of the entire world are explained.It is pointed out that the island arc and other arcuate tectonics are gradually developed under the displacement and stress fields of the arcuate tectonics and that the under-thrusting action of the ocean plate is secondary.The distance formulas between the volcanic arc and the trench are suggested and also that theoretical results are consistent with actual data.