遥感技术在高寒山区1:25万区域地质调查中的应用研究     

汪友明  尹显科  徐韬  游丽君 《四川地质学报》2003,23(2):120-122

针对高寒山区1：25万区调野外工作条件差、时间短，植被覆盖度低、遥感影像质量好的特点，提出了遥感影像解释、遥感标志剖面解译新概念，以及不同工作区用不同大法的新思路。研究、实践认为，利用遥感技术开展高寒山区区域地质调查能减少野外工作量，缩短周期，节约经费，提高调查质量和精度。  相似文献   

义敦成矿带铜银铅锌锡矿产资源调查评价进展与潜力   总被引：1，自引：0，他引：1  

林方成  杨家瑞  陈慈德  何显刚  林青  卢映祥  刘宇淳  谢恩顺 《四川地质学报》2003,23(3):141-145

义敦成矿带地处独特的大地构造部位，经历了复杂的地质构造演化和强烈的岩浆活动，成矿条件优越，矿产资源丰富。1999年实施国土资源地质大调查以来，相继发现了普朗、松诺、卓玛斑岩铜矿；砂西、热朗泽、夏隆等银铅锌矿；热隆、脚根玛锡矿；打马池觉铜金矿等一批具有重要找矿前景的矿床(点)。该地区矿产资源勘查工作程度低，蕴藏着较大的找矿潜力，有望成为国家级重要的有色及贵金属矿产勘查和开发基地。  相似文献   

新疆开展区域农业地质调查的必要性和建议     

李文铅  钟莉  王之义  李嵩龄  夏斌 《新疆地质》2003,21(4):459-462

通过对新疆农业地质资料的研究，指出了当前新疆农业地质研究方面存在的不足，阐述了区域农业地质研究的意义，提出了在新疆进行区域农业地质研究的方向、内容，以及工作部署建议．  相似文献   

数字路线地质调查与数字填图方法   总被引：5，自引：0，他引：5  

葛梦春  方成名  于庆文  李超岭 《新疆地质》2003,21(Z1):26-32

数字地质填图是基于数字填图系统(RGMAP)进行地质调查的一种新方法.从野外数字路线地质调查的角度,结合150000崇阳县幅数字填图实战经验,探讨了观察路线布置的原则和方法、PRB数字填图技术和PRB过程的基本概念,数字填图的一般工作方法和编录要求等.在此基础上对数字填图方法的长处和局限性进行了讨论.  相似文献   

高密度电法勘探在岩溶查找中的应用   总被引：10，自引：0，他引：10  

刘金涛  胡晓明 《地质科技情报》2003,22(2):100-102

介绍了武汉市汤逊湖污水处理厂厂址的地质概况和地球物理特征，以及高密度电法勘探的施工方案，分析了视电阻率异常特征，并说明了其异常验证情况。高密度电法勘探结果表明该区存在溶洞，为施工提供了决策依据，建议在有溶洞的地段采取相应措施，以防止工程建设后发生地质灾害。  相似文献   

陕西省地下水水质监测发展探析   总被引：1，自引：0，他引：1  

鱼晓利 《地下水》2003,25(1):11-12,25

本文针对陕西省地下水水质监测控制范围局限于农灌区，监测项目单一的现状，通过分析研究，提出水质监测的发展思路，剖析实现新思路的相关条件。  相似文献   

全站仪机载导线测量程序开发研究   总被引：2，自引：0，他引：2  

许承权  邹进贵  倪涵  王永弟  陈伟 《测绘信息与工程》2003,28(6):11-13

介绍了全站仪机载程序开发的重要性和必要性，基于Leica公司TPS1000／1100系列全站仪机载程序开发工具——GeoBASIC，阐述了机载导线测量程序开发的技术关键，所开发的程序达到了预期的效果，满足了用户的需求。  相似文献   

The electrical structure of the Slave craton   总被引：4，自引：0，他引：4  

Alan G. Jones  Pamela Lezaeta  Ian J. Ferguson  Alan D. Chave  Rob L. Evans  Xavier Garcia  Jessica Spratt 《Lithos》2003,71(2-4):505-527

The Slave craton in northwestern Canada, a relatively small Archean craton (600×400 km), is ideal as a natural laboratory for investigating the formation and evolution of Mesoarchean and Neoarchean sub-continental lithospheric mantle (SCLM). Excellent outcrop and the discovery of economic diamondiferous kimberlite pipes in the centre of the craton during the early 1990s have led to an unparalleled amount of geoscientific information becoming available.

Over the last 5 years deep-probing electromagnetic surveys were conducted on the Slave, using the natural-source magnetotelluric (MT) technique, as part of a variety of programs to study the craton and determine its regional-scale electrical structure. Two of the four types of surveys involved novel MT data acquisition; one through frozen lakes along ice roads during winter, and the second using ocean-bottom MT instrumentation deployed from float planes.

The primary initial objective of the MT surveys was to determine the geometry of the topography of the lithosphere–asthenosphere boundary (LAB) across the Slave craton. However, the MT responses revealed, completely serendipitously, a remarkable anomaly in electrical conductivity in the SCLM of the central Slave craton. This Central Slave Mantle Conductor (CSMC) anomaly is modelled as a localized region of low resistivity (10–15 Ω m) beginning at depths of 80–120 km and striking NE–SW. Where precisely located, it is spatially coincident with the Eocene-aged kimberlite field in the central part of the craton (the so-called “Corridor of Hope”), and also with a geochemically defined ultra-depleted harzburgitic layer interpreted as oceanic or arc-related lithosphere emplaced during early tectonism. The CSMC lies wholly within the NE–SW striking central zone defined by Grütter et al. [Grütter, H.S., Apter, D.B., Kong, J., 1999. Crust–mantle coupling; evidence from mantle-derived xenocrystic garnets. Contributed paper at: The 7th International Kimberlite Conference Proceeding, J.B. Dawson Volume, 1, 307–313] on the basis of garnet geochemistry (G10 vs. G9) populations.

Deep-probing MT data from the lake bottom instruments infer that the conductor has a total depth-integrated conductivity (conductance) of the order of 2000 Siemens, which, given an internal resistivity of 10–15 Ω m, implies a thickness of 20–30 km. Below the CSMC the electrical resistivity of the lithosphere increases by a factor of 3–5 to values of around 50 Ω m. This change occurs at depths consistent with the graphite–diamond transition, which is taken as consistent with a carbon interpretation for the CSMC.

Preliminary three-dimensional MT modelling supports the NE–SW striking geometry for the conductor, and also suggests a NW dip. This geometry is taken as implying that the tectonic processes that emplaced this geophysical–geochemical body are likely related to the subduction of a craton of unknown provenance from the SE (present-day coordinates) during 2630–2620 Ma. It suggests that the lithospheric stacking model of Helmstaedt and Schulze [Helmstaedt, H.H., Schulze, D.J., 1989. Southern African kimberlites and their mantle sample: implications for Archean tectonics and lithosphere evolution. In Ross, J. (Ed.), Kimberlites and Related Rocks, Vol. 1: Their Composition, Occurrence, Origin, and Emplacement. Geological Society of Australia Special Publication, vol. 14, 358–368] is likely correct for the formation of the Slave's current SCLM.  相似文献   

青藏高原1∶25万区域地质调查地貌年代学研究   总被引：1，自引：0，他引：1       下载免费PDF全文

柏道远  贺春平  吴能杰  罗灵生 《沉积与特提斯地质》2003,23(2):23-27

高原隆升及剥蚀作用的复杂性与区域差异性以及高原恶劣的气候、地理条件,使得在青藏高原空白区1∶25万区域地质调查中进行地貌年代学研究具有很大的现实意义.由于地貌是高原隆升、环境演化、新构造运动等的信息载体,地貌年代有助于重塑这些地质作用的发生时间及发展过程,因此地貌年代学研究具有重要的技术意义.1∶25万银石山幅的工作表明,地貌年代学调查对高原隆升及环境演化过程研究具有良好效果.  相似文献   

Spatial Database of Geological Survey Extent in 20th Century in China     

WangQuanming YeTianzhu FangYiping ChenJianguo LiShuyu ZhangDaquan 《中国地质大学学报(英文版)》2003,14(3):220-226

During the whole 20th century in China, especially the latest 50 years, we have gotten much geological information about geological mapping, geophysics, geochemistry, mineral exploration,remote sensing, environmental geology, hydrogeology, engineering geology and oceanic geology etc. by our geologists and explorers. All the information has been accmnulated and can be used as a dcision-making foundation for the future plan of geological survey. The spatial database of geological survey ex-tents has been established by using computer technology. The database contained all kinds of exploration sections and collected about 160 000 records in this database. This paper introduces the data construc-tion ,contents and applying systemof this database, and trys to let people know what kinds of geological survey were finished, when the exploration were carried out, and how and where you can get this infor-mation.  相似文献