Tectonic Characteristics and Evolution of Bohai Bay Basin, China     

LIU Pengju  ZHANG Meisheng  SUN Xiaomeng  YANG Baojun 《世界地质(英文版)》2002,5(1)

Synthetical analyzing the deep geophysical data within Bohai bay basin the authors detect the deep crustal structure presenting high geothermal flux, thinned crust and arched Moho discontinuity, and the basin basement belongs to rigid continental crust. The development of the basin was controlled by two - dimensional faults in NNE and NWW directions. The tectonic units of the basin can be subdivided into three structural divisions: the east, middle and west division. The basin is considered as a continental rift. The tectonic background and regional right - lateral stress field during the late Cretaceous and Paleogene were a compound result of the Kula Plate W - directional subducting under Eurasia Continental Plate in 80 ～ 74Ma and the Philippine sea Plate W -directional subducting under the Eurasia Continental Plate since 60Ma, the long-rang effect of the India Continental Plate wedging into the Eurasia Continental Plate and of the Siberia Plate SE - directional relatively moving.  相似文献   

提高小概率事件预报成功率的一条途径   总被引：12，自引：3，他引：9  

彭治班  吴宝俊  江剑民  王淑静 《气象》2000,26(2):3-5

在给出小概率事件定义与评估小概率事件预报成功率参数的基础上,根据参数变换后的表达式推断,变小概率事件为条件概率下的大概率事件,是提高小概率事件预报成功率的一条途径。  相似文献   

河北省涞源县木吉村铜(钼)多金属矿田成矿物质来源探讨   总被引：1，自引：0，他引：1  

张建珍  孙爱群  王海涛  马国玺  陈志宽  王自力  陈超  王宝德  牛树银  张福祥  马宝军 《吉林大学学报(地球科学版)》2015,(1):106-118

木吉村铜(钼)矿田位于太行山脉中、北段阜平幔枝构造的北东倾伏端,涞源哑铃状杂岩体连接处西侧上盘拆离带的次级断陷盆地中,主要由斑岩型铜(钼)矿、矽卡岩型铁铜矿和外围热液脉型铅锌矿构成,是河北省目前探明的唯一大型铜(钼)多金属矿田,找矿远景巨大。鉴于矿床成矿物质来源在研究矿床成因和指导找矿中的重要作用,对木吉村矿田主要矿床矿石中黄铁矿、黄铜矿、方铅矿、辉钼矿、磁铁矿、石英和石膏等单矿物进行了硫、铅、碳、氢、氧、硅、铼等同位素测定、对比和分析。结果表明:矿田中硫同位素主值域δ34S=-3.5‰~3.2‰,主平均值为0.3‰;铅同位素206 Pb/204 Pb=15.566 0~17.072 0,平均为16.547 0,207Pb/204Pb=15.031 0~15.523 0,平均为15.258 0,208 Pb/204 Pb=36.292 0~37.375 0,平均为36.721 0;碳同位素δ13 C为-2.94‰~-2.18‰,平均为-2.62‰;硅同位素δ30 SiNBS-28值域为-0.3‰~0.2‰,平均0.0‰;辉钼矿w(Re)为(23.65~266.50)×10-6,平均值为142.33×10-6;δ18 OH2O值为-10.64‰~7.70‰,极差为18.34‰,平均值为-1.47‰,较标准岩浆水值稍低,δD值为-148.4‰~-89.0‰,极差为59.4‰,平均值为-113.7‰,略低于岩浆岩δD值域。从而认为,木吉村矿田成矿物质主要来源于地球深部,成矿溶液以岩浆水为主,部分来自大气降水。  相似文献   

胶西北金矿集中区之深部控矿构造探讨   总被引：4，自引：0，他引：4  

牛树银  孙爱群  张建珍  马宝军  王宝德  陈超  张福祥  刘成  张晓飞 《地质学报》2011,85(7):1094-1107

胶西北不足全国国土面积0.25%的成矿集中区却占有接近全国25%的黄金储量.该区不仅黄金储量巨大,而且成矿时间集中(115±5Ma),并具有矿脉延深远大于延长的特点,因此备受国内、外地质学家的广泛关注.研究认为,胶西北金矿集中区与深部控矿构造有关.华北东部地区在经历了古生代漫长的稳定地台演化阶段后,于燕山运动时期进入地...  相似文献   

Metallogenic characteristics of the region of Northwest Hebei and analysis of ore prospecting potential in its peripheries     

Aiqun Sun  Shuyin Niu  Baode Wang  Yuchou Han  Minhui Wei  Baojun Ma  Zhiyuan Zhao  Dong Xia 《中国地球化学学报》2011,30(1):1-13

The region of Northwest Hebei is an area where Au-Ag polymetallic ore depsits are concentrated in Hebei Province. There were divided the Au ore-concentrated region with the magmatic-metamorphic diamictite zone as the center and the perpheral cover-strata zone and Ag-polymetallic metallogenic zone along the line of Xuanhua-Songli-Chicheng. Research on mantle branch structure indicates that Au-Ag polymetallic ore-forming materials come mainly from the deep interior of the Earth. The ore-forming materials tend to migrate upwards through the multi-stage evolution of mantle plume, and are concentrated as ores in the favourable tectonic expansion zone of a mantle branch structure. As viewed in plane, from the center to the periphery and as viewed in space, from the lower part to the upper part there exists Au-Ag-Pb-Zn zonation, as evidenced by drilling data from a number of mines. So, there is still great potential for ore prospecting in the region of Northwest Hebei.  相似文献   

内蒙古金厂沟梁金矿的构造特征及深部找矿预测   总被引：3，自引：1，他引：2  

牛树银  王宝德  张建珍  马宝军  孙爱群  聂凤军  江思宏  陈超  张占升  刘福林  赵志远 《大地构造与成矿学》2011,35(3):348-354

燕山运动以来,华北地台北缘进入了典型的陆内伸展造山阶段,究其成因可能与地幔热柱活动密切相关.研究认为金厂沟梁是一较典型的幔枝构造(地幔热柱多级演化的第三级单元),并且是该区主要的成矿控矿构造.本文在简述其成矿构造背景、含金矿脉主要特征的基础上,重点探讨了金厂沟梁金矿的矿体展布、成矿作用、控矿构造,进而总结了成矿规律,归...  相似文献   

A New Inversion Method of Sedimentary Strata For Deriving Double Parameters and Its Applications     

GUO Hua  LIU Cai  LI Yue  YANG Baojun 《世界地质(英文版)》2002,5(1)

The inverse problem of wave equation is the importance of study not only in seismic prospecting but also in applied mathematics. With the development of the research, the inverse methods of 1 - D wave equations have been trending towards the multiple parameters inversion . We have obtained an inverse method with double -parameter, in which medium density and wave velocity can be derived simultaneously. In this paper, to increase the inverse accuracy, the method is improved as follows. Firstly, the formula in which the Green Function is omitted are derived and used. Secondly, the regularizing method is reasonable used by choosing the stable function. With the new method, we may derive elastic parameter and medium density or medium density and wave velocity. Thus, lithology parameters for seismic prospecting may be obtained.After comparing the derived values from the new method with that from previous method, we obtain the new method through which substantially improve the derived accuracy . The new method has been applied to real depths inversion for sedimentary strata and volcanic rock strata in Chaoyanggou Terrace of Songliao Basin in eastern China. According to the inverse results,the gas - bearing beds are determlned.  相似文献   

库车坳陷克拉苏构造带盐上和盐下构造变形差异及其控制因素分析     

杨克基  漆家福  马宝军  孙统  张希晨  张帅 《大地构造与成矿学》2018,(2):211-224

克拉苏构造带位于库车坳陷与南天山盆山过渡带,特殊的受力环境使其构造变形机制具有特殊性。依据最新的地震和钻井资料,并结合前人研究成果,建立了克拉苏构造带新的地震解释方案,并据此分析该地区盐上、盐下层构造变形几何形态、演化过程、形成机制等方面的差异及其控制因素。结果表明:克拉苏构造带盐下层构造变形可分为两部分,包括由基底卷入的高角度正断层后期挤压形成的反转断裂系统,以及主断裂下盘发育的次生盖层滑脱逆冲叠瓦断裂系统。盐上层构造变形为褶皱相关断层,其演化经历了基底断裂向上传递形成传播褶皱、差异压实作用诱发底辟褶皱、以及褶皱核部在持续挤压作用下形成破冲断层等多个阶段。盐下层基底卷入断裂系统形成于侏罗纪盆山过渡带伸展环境,而叠瓦式盖层滑脱断裂系统和盐上层构造变形主要形成于中新世-第四纪的挤压构造环境。盆山过渡带特殊的构造部位及在不同地质时期应力场的转换控制了盐下层构造变形机制,而盐上层构造变形受到基底断裂复活、差异沉积负荷、膏盐岩底辟上涌、挤压应力增强以及北部山前地形高差等众多因素影响,且不同演化阶段主控因素有所差异。克拉苏构造带盐下、盐上层变形机制和毗邻区带相比有较大差异,这与其特殊的构造位置以及构造应力在盐下和盐上地层向前陆方向传递的方式和距离不同等因素有关。  相似文献   

GPS连续运行参考站的网络计算模型研究     

刘小鹏  赵宝军  陈建雄 《测绘标准化》2013,(4):23-25

摘要：连续运行参考站（CORS）是未来GPS发展的重要方向,着重论述CORS系统的网络计算模型,对各种计算模型的特点进行分析与对比,并结合某省卫星定位连续运行基准服务平台的应用进行深入研究。  相似文献   

基于DOFS的水位变化下土质边坡模型稳定性试验研究     

严臖凡  朱鸿鹄  施斌  王宝军  王静 《工程地质学报》2014,22(6):1263-1270

作为实现分布式监测技术(DOFS)的重要手段,光纤感测技术近年来得到了迅速的发展。这一技术在地质灾害和岩土工程监测领域有着巨大的应用潜力。本文基于布里渊光时域分析(BOTDA)和布喇格光栅(FBG)两种感测技术,设计了土质边坡稳定性分布式监测室内模型。通过模型试验,重点研究了水位变化作用下土质边坡内部应力分布以及边坡的破坏过程,根据FBG与BOTDA的应变数据,对土质边坡稳定性进行了评价,验证了BOTDA和FBG分布式光纤感测技术应用于土质边坡变形监测的可行性。研究成果对于光纤分布式感测技术的应用研发和在多场作用下的土质边坡稳定性分析具有重要的意义。  相似文献