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1.
贵州大射电望远镜候选台址优选,需综合考虑喀斯特洼地几何条件、工程条件、地质条件、气象条件和无线电环境等因素.因上述各因素具复杂性、模糊性和难量化性等特点,本文采用模糊综合评判法进行大射电望远镜候选台址优选.经研究,大射电望远镜候选台址优评价指标可取"长短轴比、最小挖填方率、最适宜口径、洼地闭合情况、岩体结构、地质灾害、洼底水文条件、交通状况"等8个参数,综合评判结果集为"好、较好、一般、差".采用专家评定法和降半梯形分布相结合的隶属度评价模型,共选出38个大射电望远镜候选台址.它们集中分布于三大区域内:一是以平塘、紫云、惠水、罗甸、荔波为中心区域;二是以普定、安顺、镇宁为中心区域;三是以安龙、兴义和关岭为中心区域.  相似文献   

2.
FAST工程地质条件分析   总被引:1,自引:0,他引:1  
李博  郭明 《地下水》2012,(2):132-133
国家天文台500 m口径球面射电望远镜工程(即望远镜工程,FAST),是利用大窝凼(即望远镜工程台址)的喀斯特洼地为基底,建造一口径为500 m的球冠面。本文对大窝凼的地貌结构、演化历史、岩溶发育、水动力进行分析,为选址大窝凼的可行性评价和工程实际提供据参考。  相似文献   

3.
黔南平塘大窝凼洼地经国家天文台多年全国考察、多次论证后确定为世界上最大直径的射电望远镜FAST候选台址.由于投资大,环境要求高,地质勘察精度,特别是在岩溶、地下水等方面的勘察精度要求尤其高,为此本次勘察从地面地质测绘、地表综合物探、井下电磁波CT、超声波测试、钻孔注水试验、地下水连通试验、室内岩土测试等一系列综合勘探,取得较好的勘察效果,为候选台址的落实起到一定促进作用.  相似文献   

4.
王馨语  郭明  赵硕 《地下水》2012,(2):142-143,165
FAST台址区广泛分布大量岩堆,厚度大、稳定性差,如何解决台址开挖过程中岩堆的稳定性,是关系到FAST安全稳定运营和台址开挖投资控制的关键。在岩堆现场调查的基础上,通过岩土工程模型试验,探索验证洼地岩堆的特有性质,并对不同支挡方式在该种条件下的稳定性和工作性能进行实验和分析,为FAST台址区岩堆的治理设计提供依据。  相似文献   

5.
安庆长江公路大桥区域稳定性及预选桥位线方案是大桥建设前期的一项重要基础性工作。本文是利用航、卫片地质解译调查 ,分析研究拟选桥址区及其外围的地质构造特征 ,新、老断层的分布情况及其活动性 ,并进行区域稳定性评价 ;利用5 0至 90年代的航、卫片资料 ,分析评价了拟选桥址区长江岸带变迁及稳定性 ;对预选桥址区工程地质条件及优选桥位线方案进行比较与论证。  相似文献   

6.
武汉阳逻长江大桥水域工程地震勘探   总被引:4,自引:1,他引:3  
王云安  刘章捷 《地球科学》2001,26(4):388-390
武汉阳逻长江大桥桥址区的工程地质条件复杂, 采用地震反射波法和地震映射波法, 在水域进行工程地震勘探, 查明了桥址区的地质构造、地层岩性分布等工程地质问题, 并对大桥的工程地质条件作出了评价, 为桥型方案的选择提供了重要的地质依据.   相似文献   

7.
正【阅读提示】被誉为"中国天眼"的国家重大科技基础设施500米口径球面射电望远镜是具有我国自主知识产权、世界最大单口径、最灵敏的射电望远镜,其研制和建设体现了我国自主创新能力,实现了我国相关装置由跟踪模仿到集成创新的跨越。作为建设在地质环境复杂地区的国家重点工程,其选址、勘察、设计、施工甚至投入使用,都离不开地质工作。为什么会选址在偏远的岩  相似文献   

8.
正2016年7月至今,陕西省地质调查院历时近2年,在中国北纬32°湿润热带-亚热带喀斯特地貌区最北界,首次发现罕见的喀斯特地质景观—汉中天坑群,包括宁强九台山台原、南郑大垭台原、西乡细辛坝台原及镇巴三元台原4个相对独立的喀斯特系统,由天坑、洞穴、峡谷、地缝、陡崖、竖井、伏流、洼地、石林、湖泊、瀑布等527处喀斯特地貌组成。其中,口径大于500m的超级天坑2个、大型天坑7个、  相似文献   

9.
东川坝塘水库建库地质条件及防渗工程   总被引:1,自引:0,他引:1  
陈光祥 《云南地质》2004,23(2):270-272
坝塘水库是利用天然构造溶蚀洼地作库盆的注入式水库。地质条件复杂,水库地处高地震烈度区(地震基本烈度为9度),同时库盆悬托,库周是低邻谷,存在灰岩喀斯特渗漏、喀斯特塌陷、不均匀沉陷等问题。本文论述建库存在的工程地质问题和相应的工程措施进一论述。  相似文献   

10.
为深化洼地空间分布及其影响因素的认识,以云南石林县为例,在ArcGIS中基于DEM提取洼地分布及相关数据,并运用K函数(Ripley’s K)、核密度函数、缓冲区、空间叠加等分析方法,探讨了该区洼地密度分布特征及地理环境对其的影响。结果表明:研究区洼地在8 km尺度上为聚集分布模式,可划分为高密度(>6个?km-2)、中密度(5~6个?km-2)和低密度(<5个?km-2)三个区域。受多种地理环境因素影响,研究区洼地密度在不同海拔段、坡度、起伏度、地层岩石和断层缓冲区上均有差异性表现;同时,岩层节理、断层方向在一定程度上控制了洼地长轴的发育。研究区潜在水文连通性、面积—高程积分值两个指标与洼地密度呈现良好的一致性,但两个指标所反映的喀斯特洼地的地貌学意义还需进一步研究。   相似文献   

11.
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.  相似文献   

12.
Well investigated platforms have been selected in each continent, and the history of Cretaceous transgressions and regressions there is concisely reviewed from the available evidence. The factual records have been summarized into a diagram and the timing of the events correlated between distant as well as adjoining areas.On a global scale, major transgressions were stepwise enlarged in space and time from the Neocomian, via Aptian-Albian, to the Late Cretaceous, and the post-Cretaceous regression was very remarkable. Minor cycles of transgression-regression were not always synchronous between different areas. Some of them were, however, nearly synchronous between the areas facing the same ocean.Tectono-eustasy may have been the main cause of the phenomena of transgression-regression, but certain kinds of other tectonic movements which affected even the so-called stable platforms were also responsible for the phenomena. The combined effects of various causes may have been unusual in the Cretaceous, since it was a period of global tectonic activity. The slowing down of this activity followed by readjustments may have been the cause of the global regression at the end of the Cretaceous.  相似文献   

13.
The Afyon stratovolcano exhibits lamprophyric rocks, emplaced as hydrovolcanic products, aphanitic lava flows and dyke intrusions, during the final stages of volcanic activity. Most of the Afyon volcanics belong to the silica-saturated alkaline suite, as potassic trachyandesites and trachytes, while the products of the latest activity are lamproitic lamprophyres (jumillite, orendite, verite, fitztroyite) and alkaline lamprophyres (campto-sannaite, sannaite, hyalo-monchiquite, analcime–monchiquite). Afyon lamprophyres exhibit LILE and Zr enrichments, related to mantle metasomatism.  相似文献   

14.
正20140751 Guo Xincheng(Geological Party,BGMRED of Xinjiang,Changji 831100,China);Zheng Yuzhuang Determination and Geological Significance of the Mesoarchean Craton in Western Kunlun Mountains,Xinjiang,China(Geological Review,ISSN0371-5736,CN11-1952/P,59(3),2013,p.401-412,8  相似文献   

15.
正20141058 Chen Ling(Key Laboratory of Mathematical Geology of Sichuan Province,Chengdu University of Technology,Chengdu610059,China);Guo Ke Study of Geochemical Ore-Forming Anomaly Identification Based on the Theory of Blind Source Separation(Geosci-  相似文献   

16.
SEISMIC GEOLOGY     
正20141334 Chen Kun(Institute of Geophysics,China Earthquake Administration,Beijing100081,China);Yu Yanxiang Shakemap of Peak Ground Acceleration with Bias Correction for the Lushan,Sichuan Earthquake on April20,2013(Seismology and Geology,ISSN0253-4967,CN11-2192/P,35(3),2013,p.627-633,2 illus.,1 table,9 refs.)Key words:great earthquakes,Sichuan Province  相似文献   

17.
正20141624 Cai Xiongfei(Key Laboratory of Geobiology and Environmental Geology,Ministry of Education,China University of Geosciences,Wuhan 430074,China);Yang Jie A Restudy of the Upper Sinian Zhengmuguan and Tuerkeng Formations in the Helan Mountains(Journal of Stratigraphy,ISSN0253-4959CN32-1187/P,37(3),2013,p.377-386,5 illus.,2 tables,10 refs.)  相似文献   

18.
PALEONTOLOGY     
正20142263Lü Shaojun(Geological Survey of Jiangxi Province,Nanchang 330030,China)Early-Middle Permian Biostratigraphical Characteristics in Qiangduo Area,Tibet(Resources SurveyEnvironment,ISSN1671-4814,CN32-1640/N,34(4),2013,p.221-227,2illus.,2tables,22refs.)Key words:biostratigraphy,Lower Permian,Middle Permian,Tibet  相似文献   

19.
正20142560Hu Hongxia(Regional Geological and Mineral Resources Survey of Jilin Province,Changchun 130022,China);Dai Lixia Application of GIS Map Projection Transformation in Geological Work(Jilin Geology,ISSN1001-2427,CN22-1099/P,32(4),2013,p.160-163,4illus.,2refs.)  相似文献   

20.
GEOCHEMISTRY     
正20140692 Duo Tianhui(No.402 Geological Team,Exploration of Geology and Mineral Resources of Sichuan Authority,Chengdu611730,China);Wang Yongli Computer Simulation of Neptunium Existing Forms in the Groundwater(Computing Techniques for Geophysical and Geochemical Exploration,ISSN1001-1749,CN51-1242/P,35(3),  相似文献   

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