Ore mineralization related to the zone of the pre-Riphean structural-stratigraphic unconformity and Lower Riphean platform cover of the Uchur-Maya depression, the southeastern Siberian Platform     

M. V. Goroshko  V. A. Gur’yanov 《Russian Journal of Pacific Geology》2007,1(6):586-601

  相似文献   

华北地台中寒武统张夏组上部高频层序研究   总被引：8，自引：1，他引：7  

陈建强  史晓颖 《地层学杂志》1998,22(2):109-115

根据华北地台东部寒武系露头层序地层研究,将张夏组划分为两个正层序,其中上部正层序（５３０－５２５ＭａＢ．Ｐ．,三叶虫带Ａｍｐｈｏｔｏｎ－Ｔａｉｔｚｕｉａ带至Ｄａｍｅｓｅｌａ带）由４个亚层序和１７－２３个小层序组成,其中正层序和亚层序具有高分辨率区域地层对比意义。每一级层序均表现为向上变浅和变粗进积型序列,底部常以间断－加深面或洪泛面为界。该时期的海平面变化具有高频振荡特点,构成一个三级复合海平面变化旋回。由不同级别层序所反映的海平面变化旋回可以分别与天文周期的奥特周期（２—５Ｍａ）、米兰科维奇长周期（０．１—０．４Ｍａ）和米兰科维奇短周期（０．０２—０．０４Ｍａ）相对比。据层序地层和相序及相模式的研究,识别出６种类型的小层序,陆棚盆地至上缓坡显示出由Ａ—Ｆ类型的规律性变化。  相似文献   

Heat flow map of the European part of the U.S.S.R.     

R. I. Kutas  E. A. Lubimova  Ya. B. Smirnov 《Pure and Applied Geophysics》1978,117(1-2):104-108

A heat flow isoline map is presented. Low and relatively constant heat flow has been observed in the old shield areas of the East European Platform (25–40 mW/m²). Increased heat flow (>50 mW/m²) has been found in the Dniepr-Donetz depression. The area south of the East European Platform is characterized by highly variable heat flow (55–100 mW/m²). Some geophysical implications are discussed.  相似文献   

Cretaceous transgressions and regressions on the Russian Platform, in Crimea and Central Asia     

D. P. Naidin  I. G. Sasonova  Z. N. Pojarkova  M. R. Djalilov  G. N. Papulov  Yu. Senkovsky  V. N. Benjamovsky  L. F. Kopaevich 《Cretaceous Research》1980,1(4):375-387

This paper is a brief explanation of the diagrams of the Cretaceous transgressions and regressions on the Russian Platform, in the Crimea (Figures 1–3) and some regions of central Asia—the western flanks of the Tien Shan mountains, the Fergana basin, the Zeravshan-Gissar and Alaj mountains, and the Northern Pamirs (Figures 5–7).Internationally recognized stages are employed. They are interpreted by Sasonova (1967) for the Lower Cretaceous (K₁) of the Russian Platform, by Naidin (1977) for the Upper Cretaceous (K₂) of the Platform and the Crimea, by Djalilov (1971) and Pojarkova (1976) for the Upper Cretaceous of central Asia. General data on the stratigraphy of the Cretaceous of central Asia may be found in Anon 1977.  相似文献   

北京市政务地理空间信息资源共享服务平台建设实践   总被引：5，自引：4，他引：1  

李军  陈桂红  田鹏  付哲 《地理信息世界》2009,7(3):20-25

从北京市政务地理空间信息资源共享服务平台（以下简称＂平台＂）的建设背景,总体框架,关键技术及创新点、服务现状及成果,经济社会效益等方面介绍了该平台的建设实践。  相似文献   

地理信息公共服务平台地理实体数据建模研究   总被引：8，自引：3，他引：5  

蒋捷  黄蔚  卢卫华  郑新燕 《地理信息世界》2009,7(4)

围绕国家地理信息公共服务平台在线地理信息服务的需求,在分析国内外相关成果的基础上,提出了面向实体的数据建模思路,设计了地理实体数据模型,能够方便地实现地理信息与社会、经济、自然资源等专题信息的挂接,并有效解决多比例尺实体目标的一致性维护问题.  相似文献   

Hill Instability Analysis of TLP Tether Subjected to Combined Platform Surge and Heave Motions   总被引：1，自引：0，他引：1  

徐万海  曾晓辉  吴应湘  刘家悦 《中国海洋工程》2008,22(4):533-546

This paper presents the Hill instability analysis of Tension keg Platform （TLP） tether in deep sea. The 2-D nonlinear beanl model, which is undergoing coupled axial and transverse vibrations, is applied. The governing equations are reduced to nonlinear Hill equation by use of the Galerkin＇ s method and the modes superposition principle. The Hill instability charted up to large parameters is obtained. An important parameter M is defined and can be expressed as the functions of tether length, the platform surge and heave motion amplitudes. Some example studies are performed for various envirotnnental conditions. The results demonstrate that the nonlinear coupling between the axial and transverse vibrations has a significant effect on the response of structure. It needs to be considered for the accurate dynamic analysis of long TI2 tether subjected to the combined platfolna surge and heave motions.  相似文献   

中国地貌基本形态划分的探讨   总被引：16，自引：1，他引：15  

李钜章 《地理研究》1987,6(2):32-39

本文从地貌学的性质出发,确定形态分类的指导原则应着眼于反映成因的形态。运用模糊数学方法建立形态基本类型的分类系统。给出进一步划分基本形态类型的两个分类方案,并分析它们的优缺点。  相似文献   

内蒙古镶黄旗哈达庙金矿杂岩体年代学、地球化学及其形成机制   总被引：2，自引：0，他引：2  

郝百武  蒋杰 《岩石矿物学杂志》2010,29(6):750-762

在中亚造山带东段华北地台北缘,识别出一套原认为是燕山期的晚古生代哈达庙石英闪长岩,其LA-ICP-MS锆石U-Pb年龄为272.9±2.4Ma(MSWD=2.0)。哈达庙石英闪长岩及其相伴出露的哈达庙含金花岗斑岩,都具有高钾钙碱性I型花岗岩的性质,∑REE较低,LREE富集明显,具有中等到弱的铕负异常,与原始地幔相比,都具有大离子亲石元素(LILE)K、Rb、Th、Zr、Hf,轻稀土元素(LREE)La、Ce,相对高场强元素(HFSE)Nb、Ta、Ti、P富集的消减带组分(SZC)特性,并且具有陆缘弧火山岩的特征。从石英闪长岩到含Au花岗斑岩,具有板块碰撞前到同碰撞的岩石特征;通过Sr、Nd、Pb同位素分析,认为哈达庙金矿杂岩主要来源于壳、幔混源,具有新生下地壳(古岛弧带)的特征;石英闪长岩的先期熔出为贫硫化物斑岩型金矿成矿元素在花岗斑岩体内的富集创造了条件;哈达庙含金花岗斑岩异常富集易熔流体相元素(Rb、Ba、Th、U、K)可能是成矿岩体与非成矿岩体的鉴别标志。本文为在中亚造山带东段华北地台北缘寻找与古亚洲洋俯冲增生碰撞有关金矿提供了线索。  相似文献   

Contribution of SHRIMP U–Pb zircon geochronology to unravelling the evolution of Brazilian Neoproterozoic fold belts     

Miguel Angelo Stipp Basei  Benjamim Bley Brito Neves  Oswaldo Siga Junior  Marly Babinski  Marcio Martins Pimentel  Colombo Celso Gaeta Tassinari  Maria Helena Bezerra Hollanda  Allen Nutman  Umberto Giuseppe Cordani 《Precambrian Research》2010

The South-American continent is constituted of three major geologic–geotectonic entities: the homonym platform (consolidated at the end of the Cambrian), the Andean chain (essentially Meso-Cenozoic) and the Patagonian terrains, affected by tectonism and magmatism through almost all of the Phanerozoic. The platform is constituted by a series of cratonic nuclei (pre-Tonian, fragments of the Rodinia fission) surrounded by a complex fabric of Neoproterozoic structural provinces.  相似文献