矿产资源勘查区块的划分及编号简介

举例对矿产资源勘查区块的划分及编号方法进行了介绍.并按纬度差10′的间隔,计算出了安徽省不同纬度上基本单位区块、四分之一区块和小区块的面积,为在全省境内实施的矿产资源勘查项目的勘查面积计算提出了统一标准.     

勘查区块的划分,编号与面积计算

对地质矿产勘查区域进行了块划分，编号与面积计算，是探矿权管理的基础性工作。熟练掌握勘查区块的划分，编号与面积计算，对地勘工作及相应的管理工作，具重要的实际意义。本文介绍了区块划分与编号的方法，给出了快速查出我省范围内区块编号的一套表格，提出了准确计算勘查区域内各级区块面积的公式。     

安徽省重要矿产地质勘查项目区块（探矿权）设置研究

安徽省是我国矿产资源丰富的省份之一,是重要的煤炭、有色金属、建材及钢铁生产基地,矿业经济在安徽省的经济发展中占有十分重要的地位。为进一步加强探矿权管理,鼓励、支持社会资金参与矿产资源勘查开发,促进矿产资源管理健康有序发展,创新地质勘查开发新机制,实现安徽省地质找矿新的重大突破,特对安徽省重要矿产地质勘查项目区块(探矿权)设置进行研究。在安徽省矿产资源总体规划和地质勘查规划的总体框架下,对安徽省重要矿产勘查区、预留区、成果保护区的地质背景和成矿条件进行研究,进一步细化和实施地质勘查规划,突出重点矿种和重点成矿区带勘查工作,科学合理地划分勘查区块,设立矿产勘查项目区块(探矿权),为地质勘查及探矿权设置和整合提供技术依据。     

矿业权市场开始启动

为配合新矿法的实施,1998年2月12日,国务院颁布施行了《矿产资源勘查区块登记管理办法》、《矿产资源开采登记管理办法》、《探矿权采矿权转让管理办法》三个配套行政法规,对矿法的基本法律     

滕州市2008年度矿产资源勘查项目年度检查工作圆满完成

为加强探矿权管理,规范探矿人勘查行为,根据《矿产资源勘查区块管理办法》及省、市文件精神,滕州市国土资源局对滕州市持证矿产资源勘查项目进行了集中全面检查。截至2008年9月30日,滕州市辖区内结束和正在实施的矿产资源勘查项目共10个,其中煤8个,多金属矿1个,铁矿1个。2008年度共完成地质测量97．86km^2,高精度磁测40km^2,地震物探点2320个,机械岩芯钻探815m,完成勘查投入320．17万元。     

对我国矿业税费制度的思考

根据《矿产资源法》第五条有关国家对矿产资源实行有偿开采的规定,国家于1994年先后实施了《中华人民共和国资源税暂行条例》和《矿产资源补偿费征收管理规定》,开征了资源税和资源补偿费,并于1998年发布实施了《矿产资源勘查区块管理办法》、《矿产资源开采登记管理办法》,开始了对探矿权和采矿权实行有     

按照国际惯例编写矿产投资项目简介

1996年8月我国颁布修改后的《矿产资源法》和1998年2月出台的《矿产资源勘查区块登记管理办法》,《矿产资源开采登记管理办法》和《探矿权采矿权转让管理办法》,明确了外国投资者在中国投资矿业的权利、义务和条件。使原     

浅析矿产资源所有权矿业权特征及其相互关系

伴随新修改的《矿产资源法》实施及1998年3月《矿产资源勘查区块登记管理办法》、《矿产资源开采登记管理办法》、《探矿权采矿权转让管理办法》三个行政法规的颁布,矿业权将实行有偿取得并可以转让.这样,市场经济中形成了一个新的市场——矿业权市场.为了培育、规范并管理好这个市场,     

国土资源部关于进一步规范探矿权管理有关问题的通知

各省、自治区、直辖市国土资源厅（国土环境资源厅、国土资源局、国土资源和房屋管理局、规划和国土资源管理局）：为进一步完善探矿权管理,规范探矿权市场秩序,维护探矿权人的合法权益,促进矿产资源勘查健康有序发展,依据<<中华人民共和国矿产资源法》、（《矿产资源勘查区块登记管理办法》等相关法律法规的有关规定,现就进一步规范探矿权管理有关事宜通知如下：     

四川省矿产资源勘查开发基地划分与评价

结合四川省第三轮矿产资源规划编制的需求,从地质工作程度、矿产资源要素、开发条件要素、社会经济要素和生态环境要素等5个因素划分了四川矿产资源勘查开发基地,并构建了勘查开发基地的评价指标体系,采用综合指数法对划分出的27个四川矿产资源勘查开发基地进行了评价,依据评价结果分为建设型、生产型和后备型三类。本文定性与定量分析相结合的方法,研究成果以期对四川省矿产资源勘查开发基地的划分提供支撑。     

The terrestrial fauna of the Late Triassic Pant-y-ffynnon Quarry fissures,South Wales,UK and a new species of Clevosaurus (Lepidosauria: Rhynchocephalia)

Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco.     

Définition d'une limite multicritère ; stratigraphie du passage Campanien–Maastrichtien du site géologique de Tercis (Landes,SW France)Definition of a multi-criteria boundary; stratigraphy of the Campanian–Maastrichtian interval of the geological site at Tercis (Landes,SW France)

Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414.     

The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts

The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H₂O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H₂O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species.     

Quaternary stresses revealed by calcite twinning inversion: insights from observations in the Savonnières underground quarry (eastern France)

Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ₁ roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003).     

NONMETALS DEPOSITS

正20141520 Bo Ying(Key Laboratory of Metallogeny and Mineral Assessment,MLR,Beijing 100037,China);Liu Chenglin Saline Spring Hydrochemical Characteristics and Indicators for Potassium Exploration in Southwestern and Northern Tarim Basin,Xinjiang(Acta Geoscientica Sinica,ISSN1006-3021,CN11-3474/P,34(5),2013,p.594-602,5 illus.,3 tables,28 refs.)     

MATHEMATICAL GEOLOGY

正20141243Chen Ge(Hangzhou Research Institute of Petroleum Geology,PetroChina,Hangzhou 310023,China);Si Chunsong Study on Sedimentary Numerical Simulation Method of Fan Delta Sand Body(Journal of Geology,     

PROSPECTING EXPLORATION

正20142599Chen Sanming(Guangxi Key Laboratory of Concealed Deposits Exploration,Guilin University of Technology,Guilin541004,China);He Yuzhou Block Model and Reserves Estimation of Panzhihua Iron Deposit Based on 3D Geological Modeling(Journal of Guilin University of Technology,ISSN1674-9057,CN45-1375/N,33(4),2013,p.610-615,9illus.,1table,15refs.)     

STRUCTURAL GEOLOGY

正20140594 Bai Daoyuan(Hunan Institute of Geology Survey,Changsha 410016,China);Zhong Xiang Faults in the Jingzhou Basin and Their Tectonic Settings(Geotectonica et Metallogenia,ISSN1001-1552,CN44-1595/P,37(2),2013,p.173-183,6illus.,59refs.)Key words:basin evolution,tectonic setting,South China In the Upper Paleozoic and Jurassic se-     

STRUCTURAL GEOLOGY

正20141912Cao Hui(State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China)Gravitational Collapse and Folding during Orogenesis:A Comparative Study of FIA Trends and Fold Axial Plane Traces(Geology in China,ISSN1000-3657,CN11-1167/P,40(6),2013,p.1818-1828,9illus.,35refs.,with