全文获取类型
收费全文 | 13272篇 |
免费 | 2964篇 |
国内免费 | 6973篇 |
专业分类
测绘学 | 120篇 |
大气科学 | 15篇 |
地球物理 | 375篇 |
地质学 | 20984篇 |
海洋学 | 315篇 |
天文学 | 6篇 |
综合类 | 1106篇 |
自然地理 | 288篇 |
出版年
2024年 | 138篇 |
2023年 | 445篇 |
2022年 | 595篇 |
2021年 | 610篇 |
2020年 | 589篇 |
2019年 | 660篇 |
2018年 | 586篇 |
2017年 | 728篇 |
2016年 | 884篇 |
2015年 | 890篇 |
2014年 | 1186篇 |
2013年 | 939篇 |
2012年 | 1178篇 |
2011年 | 1099篇 |
2010年 | 1027篇 |
2009年 | 883篇 |
2008年 | 820篇 |
2007年 | 910篇 |
2006年 | 851篇 |
2005年 | 746篇 |
2004年 | 736篇 |
2003年 | 670篇 |
2002年 | 624篇 |
2001年 | 716篇 |
2000年 | 650篇 |
1999年 | 607篇 |
1998年 | 571篇 |
1997年 | 542篇 |
1996年 | 486篇 |
1995年 | 409篇 |
1994年 | 371篇 |
1993年 | 260篇 |
1992年 | 223篇 |
1991年 | 169篇 |
1990年 | 101篇 |
1989年 | 108篇 |
1988年 | 70篇 |
1987年 | 55篇 |
1986年 | 35篇 |
1985年 | 18篇 |
1984年 | 5篇 |
1983年 | 5篇 |
1982年 | 1篇 |
1981年 | 1篇 |
1980年 | 1篇 |
1979年 | 2篇 |
1978年 | 5篇 |
1977年 | 3篇 |
1973年 | 1篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
31.
32.
通过对个旧锡矿阿西寨矿段地表基岩的地球化学勘查。发现其成矿元素的地球化学异常表现出明显的环状分带,并以测区内隐伏花岗岩凸起为中心,元素分带序列与元素本身的地球化学性质所决定的侧向迁移活动能力相符合。该现象再次证实个旧锡矿为花岗岩岩浆期后热液成矿,花岗岩是大多数成矿金属元素的物质来源,同时也是成矿热液活动的主要驱动营力。分析认为,阿西寨测区是一个相对较完整和独立的(凸起)成矿场,成矿热液活动以阿西寨凸起为中心。成矿热液活动体系受断裂导流影响,在以花岗岩凸起为中心的分带控制下,可能存在的工业矿体将在主干断裂附近和有利的构造岩性界面产出。 相似文献
33.
通过对我国主要金矿类型中黄铁矿导电类型的分析表明,黄铁矿“电子。空穴心”与金矿床的成因类型具有密切的联系,华北地台太古代变基性火山岩中的金矿床(绿岩带型)、热水淋滤型(卡林型)金矿床,黄铁矿多为单一的“电子心”型导电。大多数产于中生代岩体中的中深脉状金矿、火山次火山岩中的金矿床,黄铁矿为“电子心”、“空穴心”混合型导电,个别的为单一的“空穴心”导电。黄铁矿的“电子.空穴心”受杂质成分As、Co、Nl在成矿背景中的丰度,进入黄铁矿品格中的替代能力的差异、补偿类质同象现象、成矿时温度以及.f(S2)等多种因素的耦合制约。 相似文献
34.
35.
36.
37.
The impact of hydrological changes on travertine deposits related to thermal springs in the Pamukkale area (SW Turkey) 总被引:2,自引:0,他引:2
Dilsiz Cüneyt Marques José Manuel Carreira Paula Maria Mimo 《Environmental Geology》2004,45(6):808-817
Pamukkale thermal waters (35 °C), exhibiting calcium-bicarbonate-sulfate composition and high carbon dioxide concentration, are of a predominantly meteoric origin. The meteoric fluid, circulating through faults and fractures, is heated by magmatic intrusions at great depth, and ascends from deep reservoirs to the surface. Mixing with relatively cold groundwater in the near surface zone promotes different saturation conditions with respect to calcium carbonate that later precipitates at depth and/or the surface. Dissolution-deposition processes of calcium carbonate both at surface and depth environments may help to reconstruct past climate direction in the field. During wet climate conditions a high-rate of calcium carbonate accumulation would be expected to occur at the surface because thermal fluid would be under-saturated with respect to calcium carbonate at depth because of a relatively higher mixing ratio with cold groundwater. During dry climate conditions the thermal fluid would be super-saturated at depth because of the highly acidic environment. Hydrometeorological studies reveal that the annual precipitation at the Pamukkale hydrothermal field tends to decrease with time. This climatic change in the area was also detected from geological records. While humid climate conditions prevailed during the late Quaternary, the area has recently been affected by arid/semi-arid climate conditions, followed by some episodic transitions. This study has shown how the system has possibly reacted to different climate conditions since antiquity. 相似文献
38.
ZHAO Pengda 《中国地质大学学报(英文版)》2004,15(3):245-252
“Three-component” method consists of three clase-connected aspects: geological anomaly,diversity of mineralization and mineral deposit spectrum. All these three concepts are not new separately, but it is a new approach to combine these three aspects in one single concept for quantitative mineral resources prediction and assessment and it is also the first time to conduct a more detailed study in each aspect. Investigation and clarification of geological anomalies, diversity of mineralization and spectrum of mineral deposits are realized by digitization and quantification of ore forming controlling factors, oreexisting symbols or marks, characteristics of mineralization and regulation of ore-genesis and laws of distribution. These procedures lead to construction of a “digital model“ for mineral resources prediction andassessment. 相似文献
39.
An experimental study on reduction of U (Ⅵ) by anaerobic bacteria, Shewane//a putrefaciens, is first reported here in China. The experimental conditions were: 35℃ and pH =7.0-7.4, corresponding to a physicochemical environments in which the sandstone-hosted interlayer oxidation-zone type uranium deposit formed in Northwest China's Xinjiang. Bacteria adopted in the present experiment, Shewanella putrefaciens, occur extensively in natural environment. Our study shows that nano-crystal precipitates of uraninite quickly occurred on the surface of the cells within one week. It was found that the pitchblende was characterized by a random arrangement of uraninite nanocrystals (2-4 nm) in it, significantly different from natural pitchblende in which uraninite nanocrystals are arranged in order. Finally, a possible mechanism of uranium biomineralization by microorganisms in the deposits is discussed. Our investigation may supply a technical train of thoughts for bioremediation of nuclear-contaminated water environments and for underground dissolving extraction of the sandstone-hosted uranium ores. 相似文献
40.
文章介绍区域地质背景、矿区地物化特征,对成矿时代、流体包裹体特征进行初步研究,并指出找矿远景,希望对矿区的矿产勘查具有借鉴和指导意义。 相似文献