全文获取类型
收费全文 | 1078篇 |
免费 | 418篇 |
国内免费 | 1011篇 |
专业分类
测绘学 | 36篇 |
大气科学 | 180篇 |
地球物理 | 271篇 |
地质学 | 1623篇 |
海洋学 | 59篇 |
天文学 | 119篇 |
综合类 | 151篇 |
自然地理 | 68篇 |
出版年
2021年 | 3篇 |
2018年 | 2篇 |
2017年 | 3篇 |
2016年 | 4篇 |
2015年 | 18篇 |
2014年 | 4篇 |
2013年 | 10篇 |
2012年 | 6篇 |
2011年 | 204篇 |
2010年 | 138篇 |
2009年 | 138篇 |
2008年 | 49篇 |
2007年 | 95篇 |
2006年 | 180篇 |
2005年 | 222篇 |
2004年 | 484篇 |
2003年 | 269篇 |
2002年 | 149篇 |
2001年 | 131篇 |
2000年 | 75篇 |
1999年 | 48篇 |
1998年 | 46篇 |
1997年 | 44篇 |
1996年 | 27篇 |
1995年 | 23篇 |
1994年 | 20篇 |
1993年 | 47篇 |
1992年 | 41篇 |
1991年 | 7篇 |
1990年 | 4篇 |
1989年 | 5篇 |
1988年 | 2篇 |
1987年 | 6篇 |
1984年 | 1篇 |
1976年 | 1篇 |
1956年 | 1篇 |
排序方式: 共有2507条查询结果,搜索用时 15 毫秒
101.
Tectonic Evolution of the Himalayan Collision Belt 总被引:5,自引:0,他引:5
Cui Junwen Institute of Geology Chinese Academy of Geological Sciences Beijing 《《地质学报》英文版》1997,71(2):133-143
This paper discusses the tectonic divisions of the Himalayan collision belt anddeals with the tectonic evolution of the collision belt in the context of crustal accretion in thefront of the collision belt, deep diapirism and thermal-uplift extension and deep material flow-ing of the lithosphere-backflowing. Finally it proposes a model of the tectonic evolution-progressive intracontinental deformation model-of the Himalayan belt. 相似文献
102.
Mineralization Ages of the Jiapigou Gold Deposits,Jilin 总被引:1,自引:0,他引:1
Li Junjian Shen Baofeng Mao Debao Li Shuangbao Zhou Huifang Cheng Yuming Tianjin Institute of Geology Mineral Resources Chinese Academy of Geological Sciences Tianjin Nonferrous Metal Geological Exploration Bureau Changchun Jilin 《《地质学报》英文版》1997,71(2):180-188
The Jiapigou gold deposits are typical vein type deposits associated withArchaean greenstone belts in China. According to the crosscutting relationships between dykesand auriferous veins, single hydrothermal zircon U-Pb dating and quartz K-Ar,~(40)Ar-~(39)Ar andRb-Sr datings, the main mineralization stage of the Jiapigou deposit has been determined to be2469-2475 Ma, while mineralization superimposition on the gold deposit occurred in1800-2000 Ma and 130-272 Ma. They form a mineralization framework of one oldermetallogenic epoch (Late Archaean-Early Proterozoic) and one younger metallogenic epoch(Mesozoic) of gold deposits in Archaean greenstone belts in China. 相似文献
103.
Spatial-temporal Frame,Evolution and Mineralization of the Northern Qilian Metallogenic Province 总被引:1,自引:0,他引:1
Sun Haitian Wu Jieren Li Jinping Institute of Mineral Deposits Chinese Academy of Geological Sciences Beijing Xi''an Institute of Geology Mineral Resources Chinese Academy of Geological Sciences Xi''an Shaanxi Institute of Mineral Deposits Chinese Academy of Geological Sciences Beijing 《《地质学报》英文版》1997,71(2):204-216
Four metallogenic epochs occurred in different tectonic environments during theevolution of the Northern Qilian metallogenic province through the geological time. The Mid-dle Proterozoic metallogenic epoch witnessed the tectonic environment of crustal breakupcaused by mantle diapirism, in which ultramafic-mafic rocks were intruded along beep faultbelts and the superlarge Jinchuan magmatic Cu-Ni sulphide deposit was formed. In theMiddle-Late Proterozoic metallogenic epoch the crust was further broken to form anintracontinental rift, in which the Chenjiamiao style massive Cu-Fe sulphide deposits hosted bybasic volcanic tuff were formed in the lower volcano-sedimentary sequence, while the largesedex type Jingtieshan style Fe-Cu deposits were formed within the upper abyssal carbon-richargillaceous sedimentary sequence. The Early Palaeozoic saw the aulacogen environment, with-in which the Baiyinchang style superlarge massive base and precious metal sulphide depositshosted by quartz keratophyric tuff were formed in the Middle-Late Cambrian rifted island arcand the massive Cu-Zn sulphide deposits and magmatic chromite deposits associated with theophiolite suite were formed in the Early-Middle Ordovician, and the Honggou style massiveCu-Fe sulphide deposits hosted by spilite were formed in the Late Ordovician back-arc basinenvironment. In the Late Palaeozoic-Meso-Cenozoic, the metallogenic province went into anintracontinental orogenic stage characterized by compressive tectonic environment, in whichthere occurred carbonate-quartz vein type and tectono-alteration gold deposits associated withductile-shear structures. 相似文献
104.
Yixunite and Damiaoite—A Twin of New Native Alloys of Indium and Platinum from the Yanshan Mountains
Yu ZuxiangInstitute of Geology Chinese Academy of Geological Sciences Baiwanzhuan Beijing 《《地质学报》英文版》1997,71(4):480-485
Yixunite and damiaoite Were found in a cobalt- and copper-bearing platinum ore vein of a contact metasomatic deposit. The chief ore minerals are bornite, chalcopyrite, magnetite and carrollite. The platinum minerals include moncheite, sperrylite, daomanite, cobalt malanite and cooperite. Yixunite and damiaoite occur as immiscible globules, 1.0 to 2.0 mm in diameter. Yixunite is always in the central part of a globule. It is opaque with metallic lustre, bright white colour and black streak. HM = 5.8; VHN50 = 634 kg/mm2 (573-681 kg/ mm2); insoluble in HCl, HNO3, HF or H3PO4; no cleavage; no magnetism. Density is hard to measure because of small grain size. Calculated density = 18.21 g/cm3. Reflective colour is bright white with a yellowish tint. Isotropic. The mean analytical results (ranges) (%) are: Pt 82.8 (81.8-83.6), In 16.4(15.6-17.1) and total 99.2. The empirical formula (based on 4 atoms) is Pt2.993 In1.007 . The five strongest lines of X-ray diffraction (hkl, d,I) are 111, 2.30 (100); 200, 1.99 ( 相似文献
105.
Yu ZuxiangInstitute of Geology Chinese Academy of Geological Sciences Baiwanzhuang Beijing 《《地质学报》英文版》1997,71(4):486-490
Changchengite occurs in chromite orebodies in dunite and in platinum placer deposits in chromite orebodies nearby. The mineral occurs as massive aggregates or veinlets on margins of iridisite (IrS2) and replaces it. Opaque. Lustre metallic. Colour steel-black. Streak black. Hm = 3.7. VHN20= 165 kg/ mm2. Isotropic. Cleavage none. Density 11.96 g/ cm3. Seven electron microprobe analyses give the following mean chemical results (wt. %): S 7.2, Cu 0.3, Te 0.4, Ir 41.2, Pt 2.8 and Bi 47.3 with total 99.1. The simplified formula is IrBiS. The strongest X-ray powder diffraction lines (hkl, d, I) are 210, 2.75 (70); 211, 2.51 (60); 311, 1.860 (100); 440. 1.090 (50) and 600, 1.027 (50). The X-ray powder diffraction pattern is similar to that of mayingite. After the diffraction data are indexed the mineral is determined to be cubic. The space group is P213 with a = 0.6164(4) nm, V = 0.2342 nm3 and Z = 4. 相似文献
106.
用冲绳海槽地区地质、地球物理、地球化学数据与资料,对横跨大陆边缘—大洋板块的中国东部—冲绳海槽—琉球岛弧地区进行综合研究. 根据地震体波、面波成像结果,空间与布格重力异常及磁力异常的综合解释等结果,利用调和系数法对该研究区的地壳厚度进行了计算,并对地壳属性进行分析. 同时,选择中国东部东北地区的宽甸、华北地区的汉诺坝、华南的闵溪和台湾海峡的澎湖列岛与冲绳海槽和日本岛弧的新生代玄武岩开展元素—同位素对比研究. 结果认为冲绳海槽岩石层明显减薄,上地幔低速层已达到莫霍面,在地幔中已形成交代软流层. 元素—同位素研究表明:它不同于中国东部,与琉球岛弧地区的特点也不相同. 综合分析认为:冲绳海槽地壳属于过渡型地壳,与大洋地壳的许多特点颇为相似. 相似文献
107.
108.
对中国钻孔应变台网观测到的昆仑山口西MS8.1大地震的应变阶资料的研究结果表明:① 很多观测值与静力位错理论计算值不符合;② 北方地震较活跃地区的很多台站观测到异常大的应变阶,而南方构造运动较不活跃地区的台站虽然也观测到地震波动,但是应变阶不明显. 由此推断,地震的触发(可能是动态触发)作用对远场的实际地震应变变化具有重要影响. 也就是说,远场的构造活动(可能是断层活动)是否曾被地震触发,可能决定当地的应变场变化的主要特征. 进一步对昌平台1999年3月11日张北地震与1999年11月1日大同地震的观测资料对比分析表明:断裂带的分布情况对实际地震应变变化有直接影响. 这证明观测到的异常大的地震应变阶可能是地震触发了当地的断层活动的表现. 相似文献
109.
1979年Imperial Valley地震、1989年Loma Prieta地震、1992年Landers地震、1994年Northridge地震、1995年阪神地震的地震断层面上的位错分布,满足分段的Gutenberg-地震位错 Gutenberg-Richter定律 b值Richter定律. 对于小位错,b值约为1;对于比较大的位错,b值大于1. 相似文献
110.
本文在等离子体准线性理论下研究了地球同步轨道附近哨声湍流对亚暴“种子电子”的波-电子共振相互作用. 当发生这种共振时,“种子电子”的动量分布函数经动量扩散而随时间演化,部分低能电子数减少了,而高能尾部分的相对论电子(能量大于1MeV)数增加了,说明“种子电子”得到了哨声湍流的有效加速,且哨声湍流的能量越高,其加速效率越高. 另外,哨声湍流的频率越低(或波数越小),共振电子的能量越高(或单位质量的动量越大);频率范围越宽,共振电子的能量范围越宽,被加速的电子数也越多. 磁层哨声湍流加速“种子电子” 大约在30h内就可以造成相对论电子数显著增加,这正好和大多数磁暴期间观测到的相对论电子通量的增长时间相当. 相似文献