云南镇沅外樟盆金成矿地质及地球化学特征

金矿受北西—南东向构造破碎蚀变带控制的中低温热液型。提出岩石、构造、蚀变、化探找矿标志。     

建水黑甲铁锰矿矿床成因探讨

建水县黑甲铁锰矿赋存于第四系残坡积层中,层状、似层状分布于平缓山坡及平坦低凹处,为一套含较多铁锰质结核、残块的第四系堆积矿.     

黄土地区不同类型滑坡的特征及影响因素

在对黄土地区现场考察的基础上,按黄土斜坡的结构特点对其进行了类型划分,阐述了各种类型黄土滑坡的主要特征,初步分析了影响黄土斜坡失稳的主要因素。     

导航型GPS接收机定时精度的分析

“能提供廉价并满足准确度达到或优于１μｓ的产业需求的世界范围内的时号传播”仍然是ＣＣＩＲ第７研究组的研究课题．为此，我们测量了４种型号的１３台导航星ＧＰＳ接收机输出的１ｐｐｓ与陕西天文台主钟ＵＴＣ（ＣＳＡＯＭＣ）的时间偏差．经电缆延迟和主钟相对子ＵＴＣ（ＣＳＡＯ）的钟差改正，测量结果表明，单次（采样时间约３０ｓ）定时测量的精度约为０．２μｓ，准确度为１～３μｓ；不同型号的ＧＰＳ接收机的硬件延时、测量偏倚误差和接收机噪声特性各不相同．只有测定这些接收机的时钟偏差并加以改正，才能达到准确度优于１μｓ的定时精度或时间同步精度。     

甘肃北山地区钨矿特征及找矿远景

利用甘肃北山地区近几年地质大调查工作的成果,依据找矿信息及化探异常、重砂异常的分布范围,对该区划分为6个找钨矿远景区。各远景区存在着较大的钨资源潜力,具有良好的成矿条件和特定的成矿类型。以期为矿产勘查工作提供新的找矿思路和依据。     

元阳岩甲-绿春潘家后山接触蚀变岩型金矿

本文涉及的接触蚀变岩型金矿化带受NW～近EW向绿春 黄草岭断裂控制,矿体产于该断裂以北黑云角闪正长斑岩岩体内、外接触带及其旁侧的构造裂隙发育部位,赋矿地层为上三叠统高山寨组(T3g)。大面积喜马拉雅期超浅成正长斑岩、印支期流纹斑岩 英安岩系列火山岩类与地层的内、外接触带对成矿十分有利。岩甲地段、八○八山顶、俄批后山及潘家后山等金异常是找金的有利靶区。     

Terrestrial organic matter controlling gas hydrate formation in the Nankai Trough accretionary prism, offshore Shikoku, Japan

Sediment core samples from Sites 1175, 1176, and 1178, ODP Leg 190, Nankai Trough were analyzed for sedimentary organic matter and inorganic elemental compositions to clarify geochemical conditions for the formation of gas hydrate. Low chloride concentrations and anomalously low core temperature infer the existence of gas hydrate at Site 1178. Trace amounts of gas hydrate are also suggested for Site 1176. Site 1175 does not have any significant evidence of gas hydrate, although all the three sites are within the gas hydrate stability zone. The sediment from Site 1178 is characterized by abundant terrigenous organic matter, older geologic ages, and comparatively higher maturity levels, suggesting high rates of CO₂ generation during diagenesis. The CO₂ generation potential of sediment may be one of the crucial conditions for the formation of gas hydrate.     

Distribution of landslides adjacent to the northern side of the Yarlu Tsangpo Grand Canyon in Tibet, China

This paper presents results of recent studies on distribution and category of landslides in one section of the Sichuan–Tibet Highway, adjacent to the northern side of the Yarlu Tsangpo Grand Canyon, Tibet, Southwestern China. In the tectonic setting predominated by compression and strike-slipping, active faults are dominant and result in the genesis of the great alpine relief together with fluvial incision and unloading. In this section, with a distance of about 290 km between Ranwu and Lulang, 34 landslides occurred. Among them, the 12 large and super-large landslides comprise the most dangerous part of the highway system to road users over the past 50 years. The landslides usually occurred in slopes comprised of moraine with a large thickness, fluvio-pluvial and lacustrine deposits and fractured rocks. Based on the examination of the physical geography, structural geology, Quaternary geology, stratigraphy and petrography, this paper presents the temporal-spatial distribution of landslides along the section and classification of them into three types with respect to mechanism and composites of landslides.

Ammonia images near objects with class 0 spectral energy distributions

The distribution of the sources of the Gamma-Ray Bursts (GRBs) recorded by the CGRO experiment is uniform for all directions in the sky, while the behaviour of the log N-log P suggests a space distribution of the events not homogeneous. The cosmological model can explain this result, but it cannot explain the presence of cyclotron lines in the burst energy spectra that has been observed by many experiments: the soviet KONUS experiment onboard VENERA probes, the Japanese GRBM experiment onboard GINGA satellite and, for only one candidate burst fortuitously observed, by the USA experiment A4 onboard HEAO1 satellite. In order to shed more light on this problem we present a new study of the log N-log P of the Gamma-Ray Bursts of the second BATSE catalogue.     

论中国经济区的类型与组织

根据作者对经济区概念和性质的理解,对我国现实存在的名目繁多的经济区进行了系统的归纳和类型的划分,指出了组织经济区的重要实践意义,并重点论述了如何从组织上加强对不同层次的综合经济区的规划协调和调控管理。