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881.
山城金矿为石英脉型金矿,受断裂构造控制。本文以多种地质、地球化学信息为基础,讨论该矿元素组合及其时空分布。结果表明,元素组合与一定成矿阶段和构造空间对应,并有一定载体,其中第一阶段元素组合与构造面倾角变化有关,栽体主要为石英脉,主成矿阶段元素组合与构造面走向扭动有关,载体主要为多金属矿化,进而查明了各阶段指示元素和矿体延伸方向。同时讨论了元素指示意义的局限性。 相似文献
882.
与火山—次火山—侵入—热液作用有关的金矿床分类探讨 总被引:7,自引:0,他引:7
讨论近年来在陆相火山-次火山-侵入-热液作用有关的金矿床分类中的一些争论问题。从具体资料出发,认为扩大浅成代温热注作用的范围,摒弃中温热液和高温热液矿床,以及经它们与斑岩矿床的关系是不妥当的;认为斑岩和系列是建立成矿模式,划分有产矿床的基础。 相似文献
883.
The Junggar orogen, Xinjiang, China, is an important part of the Ural-Mongolian orogen.The collisional orogenesis in this region occurred primarily in the Carboniferous and Permianwith an evolutional process of early compression and late extension. Mineralization of gold andother metals in the Junggar orogen occurred mainly in the Permian and in a few cases in theLate Carboniferous. The deposits are largely distributed in areas where collisional orogenesiswas intensive and formed in a transitional stage from compression to extension. Therefore, goldmineralization in the Junggar orogen is fully consistent with the collisional orogenesis in time,space and geodynamic setting. This indicates that the mineral deposit model of collisionalorogenesis is applicable to prospecting and study of ore deposits in the Junggar orogen.Furthermore, the factual distribution of gold and other deposits in this region is just the same asthe collisional orogenic model presents. 相似文献
884.
Selenium Enrichment in Cambrian Stratabound Gold Deposits in the Western Qinling Mountains 总被引:1,自引:0,他引:1
Liu Jiajun Open Laboratory of Ore Deposit Geochemistry Institute of Geochemistry Chinese Academy of Sciences Guiyang Guizhou Zheng Minghu Chengdu Institute of Technology Chengdu Sichuan Liu Jianming Research Centre of Mineral Resources Exploration Chinese Academy of Sciences Beijing Zhou Yufeng Gu Xuexiang Zhang Bin Lin Li Chengdu Institute of Technology Chengdu Sichuan Lu Wenquan Institute of Comprehensive Utilization of Mineral Resources Chengdu Sichuan 《《地质学报》英文版》1997,71(4):423-432
Stratabound gold deposits in the western Qinling Mountains occur in Cambrian chert formation composed of carbonaceous chert and carbonaceous slate. The distinctive chert formation provides important grounds for the mineralization and controls on the formation of gold deposits. Study shows that Se is exceptionally higher in both host rocks and gold orebodies. It may be recovered as a valuable component in ores for total utilization, and in some localities even independent Se orebodies (which are mined exclusively for Se) may be delineated. In gold ore Se mainly occurs as independent minerals or in the isomorphous form in sulphides and there is a positive correlation between Se and Au. 相似文献
885.
886.
887.
Wang Guanfu Chen Zhihong Ding Shiying Ren FugenTianjin Institute of Geology Mineral Resources Tianjin China 《《地质学报》英文版》1996,70(1):74-86
Based on palaeomagnetic studies of the Precambrian gold deposits in the Xiong'ershan area, Henan Province, the authors infer that the ore-forming processes of the Beiling alteration-type gold ore deposit and the Dianfang breccia-type gold ore deposit started in the Proterozoic, and was superimposed by later mineralization, whereas the mineralization age of the Jiguanshan quartz- vein type gold ore deposit is Yanshanian. 相似文献
888.
外生金包括砾岩金和松散砂金,是外能作用在地表开放条件下形成的。在地壳发展过程中,动力学成矿的时空演化是连续的,但主要集中在早、晚元古代及早、晚古生代和中生代,而大发展于新生代。依据演化规律和矿化环境,提出5个找矿有望的外生金成矿带。 相似文献
889.
A recent early diagenetic banded iron-manganese mud has been forming underground in a closed lead-zinc mine for approximately 40 years. The processes leading to the banded structure of the precipitate were studied during a period of 2 years. Therefore, 19 physical and chemical parameters were measured regularly in short intervals. The resulting time series were analysed with respect to the data sets of the monthly chemical analyses of the descendent mine water, the daily rainfall and the mineral content. The results reveal that the precipitated material undergoes internal self-organization due to interaction of redox, colloid-chemical, microbial, electrical and ripening processes, and not exclusively produced by seasonal fluctuations of material input. Thus, the primary banding of the material, caused by externally forced fluctuations of the redox conditions within the mine water, is reorganized after a short time. The finally observed bands are controlled by non-linear coupling of reaction and transport processes within the mud. A genetic model for the banded mineralization was developed and verified by numerical simulation. 相似文献
890.