SHRIMP U-Pb zircon age,geochemistry and Nd isotope of the Guandaoshan pluton in SW Sichuan: Petrogenesis and tectonic significance     

Li Xianhua  Li Zhengxiang  Zhou Hanwen  Liu Ying  Liang Xirong  Li Wuxian 《中国科学D辑(英文版)》2003,46(1):73-83

SHRIMP U-Pb zircon age, geochemical and Nd isotopic data are reported for the Neo-proterozoic Guandaoshan pluton in the Yanbian region, SW Sichuan. This pluton is of typical I-type granite and emplaced at (857 ± 13) Ma. Geochemical and Nd isotopic characters suggest that the pluton was generated by partial melting of pre-existing, young (late Mesoproterozoic to early Neo-proterozoic) low-K tholeiitic protolith within an intraplate anorogenic setting. The Guandaoshan pluton probably records the earliest magmatism induced by the proposed ca. 860–750 Ma mantle superplume beneath the supercontinent Rodinia.  相似文献   

Spatial probabilistic modeling of slope failure using an integrated GIS Monte Carlo simulation approach   总被引：4，自引：0，他引：4  

G. Zhou  T. Esaki  Y. Mitani  M. Xie  J. Mori 《Engineering Geology》2003,68(3-4):373-386

Spatial probabilistic modeling of slope failure using a combined Geographic Information System (GIS), infinite-slope stability model and Monte Carlo simulation approach is proposed and applied in the landslide-prone area of Sasebo city, southern Japan. A digital elevation model (DEM) for the study area has been created at a scale of 1/2500. Calculated results of slope angle and slope aspect derived from the DEM are discussed. Through the spatial interpolation of the identified stream network, the thickness distribution of the colluvium above Tertiary strata is determined with precision. Finally, by integrating an infinite-slope stability model and Monte Carlo simulation with GIS, and applying spatial processing, a slope failure probability distribution map is obtained for the case of both low and high water levels.  相似文献   

Three-dimensional stability evaluation of landslides and a sliding process simulation using a new geographic information systems component   总被引：8，自引：0，他引：8  

Mowen Xie  Tetsuro Esaki  Guoyun Zhou  Yasuhiro Mitani 《Environmental Geology》2003,43(5):503-512

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Origin and tectonic significance of a Mesozoic multi-layer over-thrust system within the Yangtze Block (South China)   总被引：21，自引：0，他引：21  

Dan-Ping Yan  Mei-Fu Zhou  Hong-Lin Song  Xin-Wen Wang  John Malpas 《Tectonophysics》2003,361(3-4):239-254

In the Yangtze Block (South China), a well-developed Mesozoic thrust system extends through the Xuefeng and Wuling mountains in the southeast to the Sichuan basin in the northwest. The system comprises both thin- and thick-skinned thrust units separated by a boundary detachment fault, the Dayin fault. To the northwest, the thin-skinned belt is characterized by either chevron anticlines and box synclines to the northwest or chevron synclines to the southeast. The former structural style displays narrow exposures for the cores of anticlines and wider exposures for the cores of synclines. Thrust detachments occur along Silurian (Fs) and Lower Cambrian (Fc) strata and are dominantly associated with the anticlines. To the southeast, this style of deformation passes gradually into one characterized by chevron synclines with associated principal detachment faults along Silurian (Fs), Cambrian (Fc) and Lower Sinian (Fz) strata. There are, however, numerous secondary back thrusts. Therefore, the thin-skinned belt is like the Valley and Ridge Province of the North American Applachian Mountains. The thick-skinned belt structurally overlies the thin-skinned belt and is characterized by a number of klippen including the Xuefeng and Wuling nappes. It is thus comparable to the Blue Ridge Province of Appalachia.The structural pattern of this thrust system in South China can be explained by a model involving detachment faulting along various stratigraphic layers at different stages of its evolution. The system was developed through a northwest stepwise progression of deformation with the earliest delamination along Lower Sinian strata (Fz). Analyses of balanced geological cross-sections yield about 18.1–21% (total 88 km) shortening for the thin-skinned unit and at least this amount of shortening for the thick-skinned unit. The compressional deformation from southeast to northwest during Late Jurassic to Cretaceous time occurred after the westward progressive collision of the Yangtze Block with the North China Block and suggests that the orogenic event was intracontinental in nature.  相似文献   

Theory and Method of Mineral Resource Prediction Based on Synthetic Information     

WangShicheng YeShuisheng ZhouDongdai 《中国地质大学学报(英文版)》2003,14(3):207-214

Metallogenic prognosis of synthetic information uses the geological body and the miaeral resource body as a statistical unit to interpret synthetically the information of geology, geophysics, geo-chemistry and remote sensing from the evolution of geology and puts all the information into one entire system by drawing up digitalized interpretation maps of the synthetic information. On such basis, differ-ent grades and types of mineral resource prospecting models and predictive models of synthetic informa-tion can be established. Hence, a new integrated prediction system will be formed of metallogenic prog-nosis (qualitative prediction), mineral resources statistic prediction (determining targets) and mlaeral resources prediction (determining resources amount).  相似文献   

南海上层海洋热结构的年循环与半年循环   总被引：7，自引：0，他引：7       下载免费PDF全文

高荣珍  王东晓  王卫强  周发琇  谢强 《大气科学》2003,27(3):345-353

根据南海季风试验(SCSMEX)期间南海内区的三个ATLAS(Autonomous Temperature Line Acquisition System)锚碇浮标资料(1998年4月～1999年4月),采用谐波分析方法对南海上层海洋水温年循环、半年循环加以分离,发现无论在年循环还是在半年循环尺度上,18°N附近SCS1站与13°N附近SCS3站的水温变化次表层与表层呈反位相;15°20′N附近SCS2站水温变化基本上次表层与表层同位相.这说明不同区域上层海洋热变化受不同的正压与斜压模态控制.其次,SCS2、SCS3两点水温年循环振幅均在次表层达到极值;而SCS1在表层达到极大值,在100 m深度达到次极大值.3个站位水温半年循环振幅极值均出现在次表层内,这说明该层内的水温半年循环在温度变化趋势中所占的权重比在表层的权重大.  相似文献   

天气学和天气预报的研究进展   总被引：14，自引：4，他引：14       下载免费PDF全文

陶诗言  赵思雄  周晓平  纪立人  孙淑清  高守亭  张庆云 《大气科学》2003,27(4):451-467

全面回顾了75年来中国科学院大气物理研究所科研人员在气团、锋面、梅雨、寒潮、阻高、副高、暴雨、高低空急流、亚澳季风区内涡旋和对流等现象的天气学研究进展及其在不同时期所取得的研究成果,总结了在短中期天气预报及短期气候预测领域在模式发展和改进以及在数值模拟等方面所取得的成就和进展.同时指出模式发展和预测在中国数值天气预报及短期气候预测方面所做出的贡献.  相似文献   

次天气尺度及中尺度暴雨系统研究进展   总被引：37，自引：8，他引：37       下载免费PDF全文

高守亭  赵思雄  周晓平  孙淑清  陶诗言 《大气科学》2003,27(4):618-627

回顾了75年来中国科学院大气物理研究所科研人员在次天气尺度及中尺度暴雨系统领域的研究工作,这些领域主要包括暴雨、中尺度低空急流、低涡、梅雨锋结构及梅雨锋生、对称不稳定和涡层不稳定以及暴雨等灾害天气的天气动力学及数值模拟研究等;总结了在次天气尺度及中尺度暴雨系统研究的不同时期所取得的成就以及这些成就在防止和减轻中尺度暴雨灾害方面所起到的重要作用.  相似文献   

ENSO动力学与预测   总被引：10，自引：2，他引：10       下载免费PDF全文

张人禾  周广庆  巢纪平 《大气科学》2003,27(4):674-688

发生在热带太平洋地区的ENSO现象是海气相互作用的集中表现,是年际气候变化中的最强信号.由于它的发生会在全球许多地区引起严重的气候异常,极大地影响着这些地区的工农业生产和人民生活,因此,对ENSO的机理及其预测的研究一直是大气海洋界的一个热点研究课题.中国科学院大气物理研究所在ENSO的机理及其预测等方面进行了大量的研究,取得了许多研究成果.作者将对中国科学院大气物理研究所在这方面的一些研究成果进行回顾和介绍.  相似文献   

一次梅雨锋降水系统三维风场双、三雷达对比研究   总被引：6，自引：2，他引：6       下载免费PDF全文

周海光  王玉彬 《气象》2003,29(5):13-17

2002年，“我国重大气候和天气灾害的形成机理与预测理论研究”项目首次启用三多普勒天气雷达组网对暴雨系统进行同步观测，作者使用MUSCAT技术对6月24日梅雨锋雨带上的一个中β系统进行了双、三多普勒雷达三维风场对比分析，表明大气中低层辐合线是此次暴雨系统的一个重要特征。  相似文献