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排序方式: 共有8453条查询结果,搜索用时 296 毫秒
291.
Leng Shuying Zheng Du Institute of Geography CAS Beijing People''s Republic of China 《地理学报(英文版)》1997,(4)
I.LandDegradationDistributionandItsCharacteristicsThefarmingpastoraltransitionalregioninsemiaridlandofnorthernChinaisthemosttypicalregionoflanddegradation,andalsotheregionwithextensivelydevelopingsandydesertification.TheextentisfromHorqinSandyLandinth… 相似文献
292.
湘西南区氧化锰矿以锰帽型氧化锰矿为主,赋矿地层为震旦系下统湘锰组。其特点是含锰点多,分布面广,矿体在地壳贫化,往下3~7m开始富集,氧化深度40m左右。 相似文献
293.
郴桂地区中大比例尺成矿预测的方法与效果 总被引:1,自引:0,他引:1
郴桂地区是南岭多金属成矿带的重要地段,地质矿产工作研究程度较高,我院在此开展了大中比例尺成矿预测研究。本文扼要介绍了本区成矿预测的基本做法和预测方法,以及其主要成果和验证效果。 相似文献
294.
本文从区域构造背景出发,根据波拉湾煤勘探区地表及钻孔资料综合分析,建立了逆冲断层F1、F2及其配套的f1、f2……构造,理顺了错综复杂的构造格局,将推覆构造理论成功地用于援外生产实践。 相似文献
295.
The Uplift of the Longmenshan Thrust Belt and Subsidence of the West Sichuan Foreland Basin 总被引:8,自引:0,他引:8
Liu Shugen Luo Zhili Dai Sulan Changlu Institute of Technology Chengdu Sichuan ChinaDennis Arne Dalhousie U niversity Canadaand C.J.L. Wilson Melbourne U niversity Australia Jiang M inxi 《《地质学报》英文版》1996,70(1):16-26
Based on fission track dating of apatite, and measurement of vitrinite reflectance of rock samples from the Longmenshan (Longmen Mountain)area and the West Sichuan foreland basin and computer modelling it is concluded that (l)the Songpan-Garze fold belt has uplifted at least by 3-4 km with an uplift rate of no less than 0.3-0.4 mm/a since 10 Ma B.P.; (2) the Longmenshan thrust nappe belt has uplifted at least by 5-6 km with an uplift rate of more than 0.5- 0.6 mm /a since 10 Ma B.P.; (3) the Longmenshan detachment belt has uplifted by 1 - 2 km at a rate of 0.016-0.032 mm/a since 60 Ma B.P.; (4) the West Sichuan foreland basin has uplifted by 1.7-3 km at a rate of 0.028-0.05 mm/a since 60 Ma B.P.; (5) the uplift rate of the area on the west side of the Beichuan-Yingxiu-Xiaoguanzi fault for the last 10 Ma is 40 times as much as that on its east side; (6) the uplifting of the the Songpan - Garze fold belt and the subsidence of the West Sichuan foreland basin 60 Ma ago exhibit a mirro-image correlation, i.e 相似文献
296.
Through a detailed study of sequence boundaries, it is concluded that sequence stratigraphy is an independent regional and transitional stratigraphic system between local lithostratigraphy and global chronostratigraphy. Therefore, a new tripartite stratigraphic classification scheme has been proposed. By combining organically the concept of sequence boundaries with the GSSP, it is suggested that the GSSP should be chosen in a conformale portion of a related sequence boundary, and the boundary established in light of this concept is defined as the Best Natural Boundary (BNB). The definition of the BNB points out the working area and stratigraphic level for the GSSP. By referring to a case study of the Permian Guadalupian/Lopingian boundary, the concept of the BNB has been elaborated in detail, and it is proposed that the BNB of the Guadalupian and the Lopingian lies between the Mesogondolella granti Zone and the Ctarkina postbitteri Zone, which is also the sequence chronostratigraphic boundary between th 相似文献
297.
Oxygen Isotope Exchange Kinetics Between Coexisting Minerals and Water in the Aral Granite Pluton of the Altay Mountains, Northern Xinjiang 总被引:2,自引:0,他引:2
Liu Wei Research Center of Mineral Resources Exploration Chinese Academy of Sciences Chinese Academy of Sciences BeijingHe Baichu Changsha Institute of Geotectonics Chinese Academy of Sciences Changsh Hunanand Chen ZhenshengYichang Institute of Geology Mineral Resources Chinese Academy of GeologicalSciences Yichang Hubei 《《地质学报》英文版》1996,70(4)
Coexisting quartz, feldspar and biotite vary widely in their δ18O values and display a remarkable 18O/16O disequilibrium relation; especially, a quartz-feldspar reversal (△ 18OQUartz_feldspar< 0) exsists in the Aral granite pluton of the Altay Mountains, northern Xinjiang. The 18O / 16O exchange reaction definitely occurred between granite and water. Initial δ18O values of the granite and exotic fluid are evaluated by the mass balance consideration. The conventional method of discrimination between various magma derivations simply with δ18O values of either whole rock or separate minerals is misleading and unreliable. Experiments carried out by the authors show that the 18O / 16O exchange reaction is not accompanied by what geologists describe as petrological and mineralogical alteration effect. This decoupling relation implies that exchange reaction occurs at a relatively high temperature during subsolidus-postmagmatic cooling of magmas. The exchange mechanism is mainly diffusion-controlled. It is 相似文献
298.
南极乔治王岛中——新生代岩浆岩Sr—Nd—Pb同位素组成及源区特征 总被引:7,自引:1,他引:7
对乔治王岛11个火山岩和2个侵入岩样品做了Sr-Nd-Pb同位素分析,其中(87Sr/86Sr)i=0.70326~0.70392,εNd=3.02~6.72,206Pb/204Pb=17.776~18.515,207Pb/204Pb=15..506~15.571,208Pb/204Pb=37.868~38.308。根据以上同位素组成及其相互关系并结合岩石学和微量元素特征及火山岩中熔融包裹体成分,得出以下结论:(1)研究的乔治王岛岩浆岩起源于亏损地幔(DMM)和地幔流体交代成因的富集地幔EMI混合形成的源区;(2)该源区具有广义Dupal异常,它正是由于EMI组份加入即通过流体交代作用而产生的;(3)流体主要是俯冲深海沉积物脱碳酸盐作用而释放出的富CO2流体。 相似文献
299.
导水裂隙带高度预测途径探讨 总被引:3,自引:0,他引:3
导水裂隙带高度是设计防水煤(岩)柱尺寸的主要技术参数,是煤矿防治水工作的重要内容。详细论述了其研究现状及发展趋势,并提出了履岩体地质环境,履岩体力学环境和数值模拟技术三位一体的综合预测评价方法。 相似文献
300.