探讨矿业权经济意义加强矿业权市场建设   总被引：2，自引：0，他引：2  

张婷婷  李守义  孙英男  柴璐 《吉林地质》2006,25(2):84-88

本文探讨了矿业权价值及矿业权流转的问题,并针对目前矿业权的取得方式不够规范、矿业权流转过程中市场难以起到调节资源供需作用,以及国有地勘单位拥有探矿权的比例在不断下降等问题,提出了规范矿业权的取得方式、培育和加强矿业权市场、维护地勘单位在矿业权市场中的主体地位等建议。  相似文献   

吉林省前寒武纪地层   总被引：3，自引：1，他引：3  

周晓东  朱殿义  孙永杰 《吉林地质》2006,25(3):1-10

吉林省前寒武纪地层可见有太古宙变质表壳岩系、古元古代中深变质火山-沉积岩系、吉南新元古代陆源碎屑岩-碳酸盐岩组成的盖层沉积岩系和吉北造山带新元古代变质火山-沉积岩系4种类型.其中太古宙地层龙岗陆块具有多陆块拼贴的特点,可划分为龙岗岩群(四道砬子河岩组、杨家店岩组)、夹皮沟岩群(三道沟岩组、老牛沟岩组)、板石沟岩群、南岗岩群(鸡南岩组、官地岩组)、清原岩群.分别代表白山镇地块、夹皮沟镇地块、板石沟地块、和龙地块和清原地块的变质表壳岩系,其中除龙岗岩群可能为中太古代外,其余地质体的时代均为新太古代.古元古代地层有集安岩群、光华岩群和老岭岩群,前两者为古元古代早期裂谷环境沉积,分别可进一步划分为蚂蚁河岩组、荒岔沟岩组、大东岔岩组、双庙岩组和同心岩组,沉积时限为2 300～2 100Ma;后者为古元古代晚期内克拉通凹陷沉积,可进一步划分为林家沟岩组/达台山岩组、珍珠门岩组、花山岩组、临江岩组和大栗子岩组,沉积时限为1 900～1 800Ma.吉南新元古代地层的岩石地层学属性基本清楚,按新元古代三分的观点,其中细河群及其以下地层时代为青白口纪.浑江群时代为震旦纪,吉南地区缺失南华系.吉林省北部造山带中沿色洛河-海沟-青龙村-江域一线的元古宙地层事实上为不同时代、不同性质的构造岩片堆叠体,属于构造地层学范畴;具有层状地层特征的仅有敦化地区的塔东岩群、蛟河地区的新兴岩组、九台地区的机房沟岩群、辽源地区的西保安岩组以及安图地区的万宝岩组,时代可暂置于新元古代.  相似文献   

What Happened in the Trans-North China Orogen in the Period 2560-1850 Ma？   总被引：5，自引：0，他引：5  

Guochun ZHAO LIU Shuwen Min SUN LI Sanzhong Simon WILDE Xiaoping XIA Jian ZHANG Yanhong HE 《《地质学报》英文版》2006,80(6):790-806

The Trans-North China Orogen （TNCO） was a Paleoproterozic continent-continent collisional belt along which the Eastern and Western Blocks amalgamated to form a coherent North China Craton （NCC）. Recent geological, structural, geochemical and isotopic data show that the orogen was a continental margin or Japan-type arc along the western margin of the Eastern Block, which was separated from the Western Block by an old ocean, with eastward-directed subduction of the oceanic lithosphere beneath the western margin of the Eastern Block. At 2550-2520 Ma, the deep subduction caused partial melting of the medium-lower crust, producing copious granitoid magma that was intruded into the upper levels of the crust to form granitoid plutons in the low- to medium-grade granite-greeustone terranes. At 2530-2520 Ma, subduction of the oceanic lithosphere caused partial melting of the mantle wedge, which led to underplating of mafic magma in the lower crust and widespread mafic and minor felsic volcanism in the arc, forming part of the greenstone assemblages. Extension driven by widespread mafic to felsic volcanism led to the development of back-arc and/or intra-arc basins in the orogen. At 2520-2475 Ma, the subduction caused further partial melting of the lower crust to form large amounts of tonalitic-trondhjemitic-granodioritic （TTG） magmatism. At this time following further extension of back-arc basins, episodic granitoid magmatism occurred, resulting in the emplacement of 2360 Ma, -2250 Ma 2110-21760 Ma and -2050 Ma granites in the orogen. Contemporary volcano-sedimentary rocks developed in the back-arc or intra-are basins. At 2150-1920 Ma, the orogen underwent several extensional events, possibly due to subduction of an oceanic ridge, leading to emplacement of mafic dykes that were subsequently metamorphosed to amphibolites and medium- to high-pressure mafic granulites. At 1880-1820 Ma, the ocean between the Eastern and Western Blocks was completely consumed by subduction, and the dosing of the ocean led to the continent-arc-continent collision, which caused large-scale thrusting and isoclinal folds and transported some of the rocks into the lower crustal levels or upper mantle to form granulites or eclogites. Peak metamorphism was followed by exhumation/uplift, resulting in widespread development of asymmetric folds and symplectic textures in the rocks.  相似文献   

U-Pb Zircon Dating of the Granitic Conglomerates of the Hutuo Group： Affinities to the Wutai Granitoids and Significance to the Tectonic Evolution of the Trans-North China Orogen   总被引：3，自引：0，他引：3  

Jian ZHANG  Guochun ZHAO  LI Sanzhong  Min SUN  LIU Shuwen  Xiaoping XIA  Yanhong HE Department of Earth Sciences  The University of Hong Kong  Pokfulam Ro  Hong Kong College of Marine Geosciences  Ocean University of Chin  Qingdao  Shandong 《《地质学报》英文版》2006,80(6):886-898

1 Introduction The North China Craton (NCC) is considered to be the oldest and largest cratonic block in China. Recent studies to gain understanding of basement architecture of the NCC has led to its division into the Western and Eastern Blocks, separated by a N-S trending Paleoproterozoic Trans-North China Orogen (TNCO) (Fig. 1; Zhao et al., 1998, 1999a, 2000a, 2001a; Wilde et al., 2002). Although there is now abroad consensus that the final assembly of the NCC was completed by th…  相似文献   

测井数据滑动窗关联维计算和沉积学分析     

余继峰  李增学  刘华  王玉林  孙厚敏 《地质通报》2006,(Z2)

应用滑动窗关联维计算方法对鲁北济阳坳陷某钻井剖面石炭系—二叠系陆表海沉积层段GR测井响应数据进行了分形维数计算,结果表明海侵体系域关联维数一般较小,且维数曲线振荡变化较弱,而高水位体系域则相反。这与海侵体系域形成时海平面上升的主控因素压制或掩盖了其他因素的显现有关,同时也证明测井序列分形分析能从另一个新的视角观察识别测井序列中所包含的地质信息。随着分形方法应用研究的不断开展,必将从测井数据中挖掘出更多的有用信息,指导油气等资源勘探与开发,丰富及完善测井地质学理论。相信将来分形会成为地质数据分析的标准工具。  相似文献   

河北西北部熔积岩特征及其地质意义   总被引：1，自引：0，他引：1  

白志达徐德斌  孙善平 《岩石矿物学杂志》2006,25(6):487-492

熔积岩是火山碎屑岩的一种特殊类型，由熔浆和未固结的湿沉积物两种组分掺杂混合而成。熔积岩的形成主要受炽热熔浆与未固结的湿沉积物接触时引起的淬碎或蒸汽爆炸作用以及寄主沉积物流体化作用控制，通常分布于熔岩流底部或前缘，也可分布于超浅成侵人体周围。据熔浆碎屑物的结构特征，冀西北熔积岩可分为流状和块状两种类型。流状熔积岩多是熔浆与细粒沉积物混合的结果，块状熔积岩大多与粗粒沉积物相关。正确鉴别熔积岩对确定沉积作用与岩浆作用的时序、研究盆地发展演化历史具有重要意义。  相似文献   

基于气象站资料的中国地区太阳日辐射量算法研究   总被引：2，自引：0，他引：2  

孙睿  梁璐  杨玲 《气象与环境科学》2007,30(1):24-27

现行计算水平面太阳日辐射主要有两种方式:一种是利用影响辐射的相关要素建立模型,另一种是依据实测资料进行空间插值.但后一种方法若要保证精度则需有足够多的样本.针对上述问题,利用我国不同区域67个站点的数据,在VP-RAD模型的基础上,建立了一个适用于中国地区的逐日太阳辐射算法CNR,该算法仅需要输入站点基本信息、最高最低温度和降水量.模拟结果与实际观测结果比较吻合.  相似文献   

甘肃中东部初夏一次暴雨天气过程的动力诊断   总被引：1，自引：0，他引：1  

孙玉莲  任余龙  马新荣 《干旱气象》2007,25(4):41-45

利用Micaps常规和ECWMF资料,对造成2004年5月28～29日甘肃省中东部初夏区域性暴雨过程的高、低空急流及锋区等天气系统进行分析,结果表明:(1)500hPa西风带急流轴(≥20m.s-1)从乌拉尔山中底部向巴尔喀什湖移动,其分裂的短波槽和冷空气沿急流底部向甘肃河西至青海省中部发展,为这次大降水的形成和维持提供了能量;(2)在副热带高压快速南压东退中,高压边缘的西南暖湿气流为此次降水过程提供了充沛的水汽来源;(3)垂直速度、水汽通量、水汽通量散度等物理量对此次大(暴)雨有很好的指示意义。从能量场上,总温度平流和差动平流场对这次降水过程也有重要的贡献。  相似文献   

Interdecadal Variability of the East Asian Summer Monsoon and Associated Atmospheric Circulations     

ZENG Gang  SUN Zhaobo  Wei-Chyung WANG  MIN Jinzhong 《大气科学进展》2007,24(5):915-926

Based on the National Centers for Environmental Prediction and National Center for Atmospheric Research （NCEP/NCAR） reanalysis data from 1950-1999, interdecadal variability of the East Asian Summer Monsoon （EASM） and its associated atmospheric circulations are investigated. The EASM exhibits a distinct interdecadal variation, with stronger （weaker） summer monsoon maintained from 1950-1964 （1976-1997）. In the former case, there is an enhanced Walker cell in the eastern Pacific and an anti-Walker cell in the western Pacific. The associated ascending motion resides in the central Pacific, which flows eastward and westward in the upper troposphere, descending in the eastern and western ends of the Pacific basin. At the same time, an anomalous East Asian Hadley Cell （EAHC） is found to connect the low-latitude and mid-latitude systems in East Asia, which strengthens the EASM. The descending branch of the EAHC lies in the west part of the anti-Walker cell, flowing northward in the lower troposphere and then ascending at the south of Lake Baikal （40°-50°N, 95°- 115°E） before returning to low latitudes in the upper troposphere, thus strengthening the EASM. The relationship between the EASM and SST in the eastern tropical Pacific is also discussed. A possible mechanism is proposed to link interdecadal variation of the EASM with the eastern tropical Pacific SST. A warmer sea surface temperature anomaly （SSTA） therein induces anomalous ascending motion in the eastern Pacific, resulting in a weaker Walker cell, and at the same time inducing an anomalous Walker cell in the western Pacific and an enhanced EAHC, leading to a weaker EASM. Furthermore, the interdecadal variation of summer precipitation over North China is found to be the south of Lake Baikal through enhancing and reducing strongly regulated by the velocity potential over the regional vertical motions.  相似文献   

Brief Review of Some CLIVAR-Related Studies in China   总被引：2，自引：0，他引：2  

WANG Huijun  HAN Jinping  ZHANG Qingyun  SUN Jianqi  JIANG Dabang 《大气科学进展》2007,24(6):1037-1048

The Climate Variability and Predictability （CLIVAR） program is one of the sub-programs of the World Climate Research Program （WCRP）. In this paper, CLIVAR related research in China （2003-2006） is briefly reviewed, including four major components, namely, low-frequency intraseasonal oscillations, interannual variability, decadal variations in East Asia, and global warming simulations.  相似文献