吉尔吉斯斯坦Au、Cu、Pb、Zn、W、Sn矿床潜力评价——基于1∶100万地球化学数据     

王斌  罗彦军  孟广路  张晶  张海迪  陈博  何子鑫 《物探与化探》2022,(1):58-69

吉尔吉斯斯坦是中亚天山金属成矿带的重要组成部分,矿产资源丰富,金属矿产种类齐全.吉尔吉斯斯坦国家尺度(1∶100万)地球化学填图覆盖了吉尔吉斯斯坦全境约19万km2,分析测试了69种元素,填补了吉尔吉斯斯坦国家尺度地球化学填图空白,为吉尔吉斯斯坦基础地质、矿产开发、环境保护、农业生产等多个方面研究提供了基础地球化学数据...  相似文献   

大比例尺DLG数据生产中若干问题的探讨     

付翔 《东北测绘》2013,(4):186-188

大比例尺DLG数据是数字城市地理信息平台中最重要的基础地理信息数据,对于加快城市信息化进程具有重要的保障作用。制定合理的DLG数据生产工艺流程,精确配准影像,快速构建居民地及植被要素面,二次开发辅助程序,对提高数据质量,缩短项目生产周期具有重要意义,文章就以上问题,进行了详细的探讨与实践。  相似文献   

非量测数码相机内方位元素测量研究     

喻忠伟;王金鑫 《东北测绘》2013,(2):67-68,72

阐述了非量测数码相机内方位元素的概念、测定的原理和方法,以及在成像过程中产生误差的来源。使用共线条件方程的基本原理,选取合适的模型,利用澳大利亚墨尔本大学的Australis软件解算得到内方位元素,并分析结果的可靠性。  相似文献   

基于Microstation的专题地图编辑与出版     

王磊;续玉萍;严薇 《东北测绘》2013,(2):176-178,180

通过对专题地图特点的研究,具体阐述了利用Microstation软件完成专题地图编辑与出版的技术与方法,并针对在实际生产过程中所出现的问题提出了相应的解决方案。  相似文献   

考虑多普勒参数的SAR影像距离——共面方程及其定位   总被引：1，自引：0，他引：1  

程春泉  张继贤  黄国满  张力 《遥感学报》2013,17(6):1444-1458

通过对合成孔径雷达（SAR）影像成像几何机理的分析,以传感器位置和姿态作为定向参数,构建了考虑多普勒参数的SAR影像距离—共面方程及基于该方程的SAR影像空中三角测量模型。以登封地区99景0.5 m分辨率机载非0多普勒SAR影像为试验数据,进行了单片定向、无控制点的自由网平差、稀少控制点的区域网平差及带有自检校参数的区域网平差等系列试验。与R-D模型相比,本文模型减少了定向参数的数目,实现了SAR影像与POS数据的联合平差处理,建立的带有自检校参数的SAR影像区域网平差模型,对提高稀少或无地面控制点条件下未进行（或低精度）几何定标SAR影像的区域网平差精度起到了显著作用。较少控制点条件下模型满足了丘陵和山区1∶5000/1∶10000航摄测图对空中三角测量精度的要求。  相似文献   

U – Pb zircon ages from leucogneiss in the Etheridge Group and their significance for the early history of the Georgetown region,north Queensland     

LP Black  IW Withnall  P Gregory    JHC Bain 《Australian Journal of Earth Sciences》2013,60(3):385-401

The Timbarra Tablelands pluton is an extensive (～550 km²) complexly zoned intrusion forming one of many predominantly monzogranite I‐type plutons, which constitute the Moonbi Supersuite in northern New South Wales, Australia. It comprises an outer rim of Rocky River monzogranite (Zones 1–3), an intermediate zone of Sandy Creek syenogranite (Zones 4A–4C), surrounding a core of Surface Hill syenogranite (Zones 5–7). The suite is calc‐alkaline, high‐K, and varies from mildly metaluminous to weakly peraluminous with increasing fractionation. Average Rb/Sr ratios range from 0.4 in the least evolved very coarse‐grained monzogranite (Zone 3) to 46 in the most evolved very fine‐grained biotite microgranite (Zone 6). Trace‐element modelling indicates that the observed compositional variation could have been produced by crystal fractionation. New bulk rock major‐ and trace‐element data for 71 samples are presented, and indicate that a compositional continuum exists that varies between 63 and 78 wt% SiO₂. Importantly, there is no systematic chemical variation with spatial distribution of samples from the core of the pluton to its margin, requiring multiple separate pulses of an evolving magma to explain compositional discontinuities. The pluton is interpreted to have been emplaced at mesozonal levels (～180 ± 60 MPa, 5–10 km depth) and crystallised at temperatures between 620 and 820°C under moderately oxidising conditions (log fO₂ = ‐11.5 to ‐19). The association of gold‐molybdenite mineralisation at Timbarra with moderately oxidised I‐type magmas is consistent with fractionation‐redox controls on ore‐element behaviour in magmatic systems in other studies.  相似文献   

AUSTRALIS: A new tool for the study of isotopic systems and geochronology in mineral systems     

S. H. Sie  T. R. Niklaus  D. A. Sims  F. Bruhn  G. Suter  G. Cripps 《Australian Journal of Earth Sciences》2013,60(4):601-611

AUSTRALIS (AMS for Ultra Sensitive TRAce eLement and Isotopic Studies) is a microbeam accelerator mass spectrometry (AMS) system designed for in situ microanalysis of geological samples for trace elements and radiogenic and stable isotope data. The AMS method eliminates molecular and isobaric interferences in in situ mass spectrometric measurements, opening up new opportunities in geochronology and tracer applications. Tests have been carried out for measurements of Pb, S and Os isotopes, conducted mainly at 1.5 MV accelerating voltage. In Pb and S tests, precision as high as 0.3‰ has been obtained, made possible by a fast isotope switching system to counter the effect of instabilities in the ion source and beam transport system. In trace‐element analysis, a detection limit for Au at the sub‐ppb level was obtained.  相似文献   

南海神狐海域表层沉积物稀土元素地球化学   总被引：3，自引：0，他引：3  

赵青芳  龚建明  李双林  贺行良  付少英 《海洋地质与第四纪地质》2010,(1)

南海神狐海域表层沉积物稀土元素总量变化较大,分布范围为66.8～218.3μg/g,平均值为128.1μg/g,相对接近于中国黄土(w(∑REE)=170.66μg/g);∑REE受"粒度效应"控制,主要富集于黏土质粉砂中;各类沉积物及与中国黄土、上陆壳和珠江口沉积物的稀土元素标准化曲线的变化趋势基本一致,表明这些沉积物具有相同的物源区,且具有大陆地壳性质。铈的负异常主要受陆源源区气候环境变化控制,而与海水关系不大。∑REE与CaO、CaCO3和Sr元素呈负相关,与Al2O3、K2O、SiO2呈正相关,表明稀土元素与生物作用基本无关,可能主要吸附于黏土矿物表面和赋存于陆源碎屑矿物的晶格中。  相似文献   

On the causes of pressure oscillations in low‐permeable and low‐compressible porous media     

Joachim Berdal Haga  Harald Osnes  Hans Petter Langtangen 《国际地质力学数值与分析法杂志》2012,36(12):1507-1522

Nonphysical pressure oscillations are observed in finite element calculations of Biot's poroelastic equations in low‐permeable media. These pressure oscillations may be understood as a failure of compatibility between the finite element spaces, rather than elastic locking. We present evidence to support this view by comparing and contrasting the pressure oscillations in low‐permeable porous media with those in low‐compressible porous media. As a consequence, it is possible to use established families of stable mixed elements as candidates for choosing finite element spaces for Biot's equations. Copyright © 2011 John Wiley & Sons, Ltd.  相似文献   

Analytical and numerical analyses of the load‐bearing capacity of retaining walls laterally supported at both ends     

Sylvain Plumey  Aurelio Muttoni  Laurent Vulliet  Vincent Labiouse 《国际地质力学数值与分析法杂志》2011,35(9):1019-1033

This paper investigates the load‐bearing capacity of a perfectly smooth retaining wall laterally supported at both ends assuming that the wall fails by the development of three plastic hinges. The study considers the case of a cohesionless elastic–perfectly plastic backfill with a Mohr–Coulomb yield criterion and an associative flow rule in drained conditions. A kinematically admissible soil–structure failure mechanism is proposed and compared with the conventional solutions and with results from a numerical finite element modelling. The study shows that the proposed solution and the numerical solution are in good agreement. These solutions are found to be much more favourable for the wall than the conventional solutions. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献