全文获取类型
收费全文 | 4147篇 |
免费 | 1072篇 |
国内免费 | 1866篇 |
专业分类
测绘学 | 81篇 |
大气科学 | 25篇 |
地球物理 | 131篇 |
地质学 | 6225篇 |
海洋学 | 27篇 |
综合类 | 378篇 |
自然地理 | 218篇 |
出版年
2024年 | 23篇 |
2023年 | 78篇 |
2022年 | 138篇 |
2021年 | 164篇 |
2020年 | 158篇 |
2019年 | 225篇 |
2018年 | 155篇 |
2017年 | 186篇 |
2016年 | 240篇 |
2015年 | 245篇 |
2014年 | 346篇 |
2013年 | 288篇 |
2012年 | 362篇 |
2011年 | 387篇 |
2010年 | 366篇 |
2009年 | 271篇 |
2008年 | 225篇 |
2007年 | 328篇 |
2006年 | 280篇 |
2005年 | 246篇 |
2004年 | 231篇 |
2003年 | 224篇 |
2002年 | 222篇 |
2001年 | 231篇 |
2000年 | 194篇 |
1999年 | 211篇 |
1998年 | 179篇 |
1997年 | 169篇 |
1996年 | 153篇 |
1995年 | 96篇 |
1994年 | 106篇 |
1993年 | 68篇 |
1992年 | 72篇 |
1991年 | 59篇 |
1990年 | 45篇 |
1989年 | 35篇 |
1988年 | 25篇 |
1987年 | 20篇 |
1986年 | 23篇 |
1985年 | 6篇 |
1983年 | 3篇 |
1980年 | 1篇 |
1972年 | 1篇 |
排序方式: 共有7085条查询结果,搜索用时 15 毫秒
51.
华北陆块北缘西段狼山—白云鄂博裂谷系中元古代形成的大型多金属矿床 ,是我国重要的铁、稀土、铜、铅、锌矿产地。矿床为产于沉积岩中热水沉积型多金属矿床。其形成受地层、构造控制 ,与裂谷作用有着密切的关系。裂谷系内外分支的地质环境及矿床矿种不同 ,导致矿床特征及成因具有一定差异。白云鄂博铁、稀土矿床为钾、钠、磷等含量较高的热水沉积型 ,霍各乞铜、铅、锌多金属矿床为与中基性火山岩有关的过渡热水沉积型 ,东升庙和甲生盘等铅、锌多金属矿床为热水沉积型。文中将对上述矿床分别进行论述。 相似文献
52.
Abstract: Carbonate rocks of Cambrian (18 samples) and lower-middle Ordovician (11 samples) ages from South Korea were analyzed for sulfur contents of structurally substituted sulfate (SSS) and sulfides and their δ34 S values. The δ34 S values of SSS ranging from +25.9 to +45.2 permil, are averaged as +33.6 and +33.5 permil for the Cambrian and Ordovician rocks, respectively, which indicate high δ34 S values of the Cambro-Ordovician seawater. The SSS contents in the carbonate rocks are low being 2.9 to 17.3 ppm S (averaged as 7.0 ppm S). Sulfide sulfur, on the contrary, is much abundant containing 3 to 1,880 ppm S and the δ34 S values range widely between –17.6 and +31.1 permil. Sulfide sulfur of the studied rocks excluding impure carbonates has an average content of 187 ppm S and δ34 S value of +12.8 permil (n=24). The estimated δ34 S (sulfate–sulfide) values, which range from 13.8 to 25.4 permil in general with a few exceptions from 36.5 up to 52.3 permil for some impure carbonates, may provide evidence for the persistent oceanic anoxia with its temporary recovery during the Cambro-Ordovician time.
The SSS and sulfide sulfurs have often higher δ34 S values than the Mesozoic-Cenozoic ore sulfur (Ishihara et al., 2000). Since carbonate rocks are very reactive with circulating hydrothermal ore solution, high δ34 S values of the Korean ore deposits might be caused to some extent by 34 S enrichment from the host carbonates, resulting in the low SSS contents observed. 相似文献
The SSS and sulfide sulfurs have often higher δ
53.
The Mascot–Jefferson City (M-JC) Mississippi Valley-type (MVT) deposits are in the Valley and Ridge province of the Appalachian orogen in East Tennessee. They have been a major source of zinc for the USA but their age is uncertain and thus their genesis controversial. About 10 specimens from each of 37 sites have been analysed paleomagnetically using alternating field and thermal step demagnetisation methods and saturation isothermal remanence methods. The sites sample limestones, dolostones, breccia clasts and sphalerite–dolomite MVT mineralisation from mines in the Lower Ordovician Kingsport and Mascot formations of the Knox Group. The characteristic remanent magnetisation (ChRM) is carried by magnetite in the limestones, by both magnetite and pyrrhotite in the dolostones and by pyrrhotite preferentially to magnetite in the mineralisation. Mineralized sites have a more intense ChRM than non-mineralised, indicating that the mineralising and magnetisation event are coeval. Paleomagnetic breccia tests on clasts at the three sites are negative, indicating that their ChRM is post-depositional remagnetisation, and a paleomagnetic fold test is negative, indicating that the ChRM is a remagnetisation, and a post-dates peak Alleghanian deformation. The unit mean ChRM direction for the: (a) limestones gives a paleopole at 129°E, 12°N (dp=18°, dm=26°, N=3), indicating diagenesis formed a secondary chemical remanent magnetisation during the Late Ordovician–Early Silurian; (b) dolomitic limestones and dolostone host rocks gives a paleopole at 125.3°E, 31.9°N (dp=5.3°, dm=9.4°, N=7), recording regional dolomitisation at 334±14 Ma (1σ); and (c) MVT mineralisation gives a paleopole at 128.7°E, 34.0°N (dp=2.4°, dm=4.4°, N=25), showing that it acquired its primary chemical remanence at 316±8 Ma (1σ). The mineralisation is interpreted to have formed from hydrothermal fluid flow, either gravity or tectonically driven, after peak Alleghanian deformation in eastern Tennessee with regional dolomitisation of the host rocks occurring as part of a continuum during the 20 Ma prior to and during peak deformation. 相似文献
54.
55.
区域视觉形象识别系统设计的理论与实践 总被引:6,自引:0,他引:6
目前,全国各地正在兴起区域形象设计与建设的浪潮,但如何把区域形象信息系统地传递出去,这方面的理论研究大大落后于实践。文章就区域形象信息传递的有效工具-区域视觉识别系统设计的主要内容,设计的原则,设计的基本流程等在理论与实践上作了较为详细的探讨,并就区域视觉识别系统设计方案的经济学论证作了一些有益探讨。 相似文献
56.
Bradon Ellem 《The Australian geographer》2003,34(3):281-296
This paper examines the attempt by mining management in Western Australia's Pilbara to replace mining unions—quite literally—by removing them from the processes of representation and bargaining. It analyses the way in which those unions have tried to re-place themselves, in the senses of transforming themselves in those spaces in which they were already operating and reviving themselves where they were not. Where unionists have succeeded in these engagements, it has been by working at a range of geographical scales, using the ‘power of place’ in the Pilbara and reshaping traditional geographies of union organisation. It is suggested here that many of these emergent outcomes are the result of the embeddedness of geographically specific historical structures along with new intersections of nationally and locally scaled labour politics. 相似文献
57.
试述福建顺昌南舟萤石矿地质特征 总被引:1,自引:0,他引:1
顺昌南舟萤石矿位于顺昌县埔上镇南舟村境内,1996年福建省区域地质调查队开展1:5万埔上幅区调时发现矿体,后开展普查工作表明该矿床规模大、交通方便,易于开采,现已投入开发利用。南舟萤石矿成矿地质特征在闽北丰富的萤石资源中具有一定代表性。 相似文献
58.
通过对建宁黄埠地区金矿地质特征、矿化特点、成矿地质规律的研究,认为该区成矿年龄为91Ma,提出了北西西向碎裂带为主要的含矿构造,并指出该区具有较好的找金远景。 相似文献
59.
60.
我国钴矿矿产资源及其成矿作用 总被引:10,自引:0,他引:10
钴广泛应用于军事、钢铁、电器、机械等方面,它具有亲铁亲硫的双重性,在各类岩浆岩中的分布不均匀,由超基性岩向酸性岩,钴的含量迅速降低。我国钻矿资源呈现富矿少、贫矿多的特点,并且铬矿主要分布在甘肃、青海、新疆、吉林、陕西、云南、四川等地。按照矿床形成的成矿环境、矿床岩石组合,矿床类型划分为:与镁铁质-超镁铁质岩有关的硫化物钻矿、与海相火山喷发有关的钻多金属矿、与斑岩有关的铜钻矿、与砂岩有关的钻矿、与中酸性侵入岩有关的矽卡岩铁钻矿、与风化作用有关的钴矿等六类。 相似文献