全文获取类型
收费全文 | 45518篇 |
免费 | 8325篇 |
国内免费 | 12567篇 |
专业分类
测绘学 | 3411篇 |
大气科学 | 4377篇 |
地球物理 | 7290篇 |
地质学 | 34531篇 |
海洋学 | 4054篇 |
天文学 | 3376篇 |
综合类 | 3169篇 |
自然地理 | 6202篇 |
出版年
2024年 | 229篇 |
2023年 | 661篇 |
2022年 | 1529篇 |
2021年 | 1823篇 |
2020年 | 1707篇 |
2019年 | 2174篇 |
2018年 | 1623篇 |
2017年 | 1958篇 |
2016年 | 2073篇 |
2015年 | 2192篇 |
2014年 | 2907篇 |
2013年 | 2749篇 |
2012年 | 3031篇 |
2011年 | 3100篇 |
2010年 | 2731篇 |
2009年 | 3140篇 |
2008年 | 3036篇 |
2007年 | 3157篇 |
2006年 | 3086篇 |
2005年 | 2872篇 |
2004年 | 2557篇 |
2003年 | 2416篇 |
2002年 | 2117篇 |
2001年 | 1968篇 |
2000年 | 1929篇 |
1999年 | 1741篇 |
1998年 | 1552篇 |
1997年 | 1202篇 |
1996年 | 1027篇 |
1995年 | 853篇 |
1994年 | 772篇 |
1993年 | 612篇 |
1992年 | 463篇 |
1991年 | 401篇 |
1990年 | 259篇 |
1989年 | 217篇 |
1988年 | 167篇 |
1987年 | 106篇 |
1986年 | 63篇 |
1985年 | 46篇 |
1984年 | 27篇 |
1983年 | 23篇 |
1982年 | 17篇 |
1981年 | 12篇 |
1980年 | 13篇 |
1979年 | 10篇 |
1978年 | 18篇 |
1977年 | 8篇 |
1976年 | 4篇 |
1954年 | 7篇 |
排序方式: 共有10000条查询结果,搜索用时 46 毫秒
961.
南秦岭横丹浊积岩系是一套巨厚的浊流沉积,以向南或南东倾的单斜构造产出。由下而上,该沉积层序包括深水盆地、深水浊积扇和斜坡水道3个相序。相应地,沉积物粒度变粗,厚度变大,火山质组分含量增加,凝灰层大量发育,表明横丹浊积岩系为活动型浊积岩;其古水流方向为NNW—NNE向,物源区为南侧的碧口火山岩系。另外,横丹浊积岩系内还见石英岩、重结晶大理岩成分的砾石,说明其物源还包括被动陆缘环境的沉积物。相序、组构、沉积特征和物源区综合分析表明,横丹浊积岩系为弧前盆地充填物。构筑这一弧前盆地的动力学机制是洋壳板块向南俯冲于扬子板块被动陆缘之下,时代可能晚于中晚泥盆世。 相似文献
962.
Abstract. The Hishikari epithermal gold deposit consists of the Honko-Sanjin zone and Yamada zone. On the basis of observed crosscutting relationships of veins, vein system in the Hishikari deposit was classified into the early and late veins. They differ from orientation, width, control by unconformity, the amount of displacement and structural features, but have similarity in gold grade and Au/Ag ratios. K-Ar ages are presented for the classified veins to clarify timing of fracturing and duration of mineralization.
Age determination revealed that the early veins in the Honko-Sanjin zone range from 0.86 to 1.11 Ma and that the late veins range from 0.73 to 0. 84 Ma. The economically most important mineralization in the Hishikari deposit occurred around 0.90 Ma in a very short period (about 0.05 million years).
The distribution of mineralization age in the whole Hishikari deposit, occurrences of slickensides and ground water temperatures imply that mineralization lasted longer in the southern part of the deposit. As compared the early veins with late veins, structural changes including width, strike, dip and vein characteristics occurred at around 0.85 Ma. 相似文献
Age determination revealed that the early veins in the Honko-Sanjin zone range from 0.86 to 1.11 Ma and that the late veins range from 0.73 to 0. 84 Ma. The economically most important mineralization in the Hishikari deposit occurred around 0.90 Ma in a very short period (about 0.05 million years).
The distribution of mineralization age in the whole Hishikari deposit, occurrences of slickensides and ground water temperatures imply that mineralization lasted longer in the southern part of the deposit. As compared the early veins with late veins, structural changes including width, strike, dip and vein characteristics occurred at around 0.85 Ma. 相似文献
963.
Akira IMAI 《Resource Geology》2002,52(2):147-161
Abstract: K–Ar ages of the following porphyry Cu deposits in the western Luzon arc are determined: Lobo-Boneng (10.50.4 Ma), Santo Niño (9.50.3 Ma), Black Mountain (2.10.1 Ma), Dizon (2.50.2 Ma) and Taysan (7.30.2 Ma). Microphenocrys-tic apatite in the late Cenozoic intermediate to silicic intrusions associated with porphyry Cu deposits in the western Luzon arc contains sulfur as SO3 detectable by electron probe microanalyzer. Sulfur is supposed to have been accommodated dominantly as oxidized species in oxidizing hydrous magmas that generated porphyry Cu deposits. Likewise, such high SO3 contents in microphenocrystic apatite are common characteristics of the intermediate to silicic magmatism of the western Luzon arc, from tonalitic rocks of the Luzon Central Cordillera of about 15 Ma to an active magmatism at Mount Pinatubo. Thus, the western Luzon arc has been generating porphyry Cu mineralization associated with oxidizing hydrous intermediate to silicic magmatism related to eastward subduction, since Miocene to the present day. Intermediate to silicic rocks since 15 Ma to present-day western Luzon arc generally show high whole-rock Sr/Y ratio ranging from 20 to 184. However, porphyry Cu deposit is not necessarily related to the rocks that show higher Sr/Y ratios compared to the other barren rocks in the western Luzon arc. The characteristics of the intermediate to silicic magma associated with porphyry Cu deposit are not attributed to the composition of the source material of the magma, but to the properties defined by the high activity of oxidized species of sulfur in the fluid phase that is encountered during the generation of intermediate to silicic magmas. 相似文献
964.
Based on the mineral and chemical compositions of spoils taken from the Shilu Cu-Mo deposit and Hetai gold deposit, the leaching and batch experiments were made on spoils taken from these two deposits using the leaching column designed by the authors. The experimental results showed that it is not always true that the mine drainage is acidic. Its acidity depends on acid-buffering capacity of gangue, host rock and its alteration mineral assemblage. The composition of the drainage water is related with the interaction between superficial or underground water and solid materials in the spoils, including minerals, hydroxides and amorphous substances. The leaching extent of the element is related with its occurrence form in the deposit. The preferential flow results in leaching-out of heavy metals in large amounts. So it is important to prevent the generating of preferential flow in the system. The results will provide very important grounds for the comprehensive management of land and ecological rehabilitation of the mine site. 相似文献
965.
966.
967.
科技期刊发展的挑战与机遇 总被引:3,自引:0,他引:3
中国加入世贸组织后 ,面对开放的世界性大市场的直接冲击 ,我国出版发行行业的竞争必将更加激烈。优胜劣汰 ,会直接考验每个出版社、每份期刊。为了使我国的期刊在竞争中成为胜者 ,探讨了科技期刊参与竞争的困难与优势 ,提出了如何提高我国科技期刊竞争力的粗浅看法 相似文献
968.
969.
970.
Introduction Bohai Bay, along with its adjacent areas, is one of the seismically active areas in North China. Understanding its crust/upper-mantle structural characteristics and lateral heterogeneity of the medium in this area is of great significance to the study of seismogenic environment, thus improvimg the level of earthquake prediction. For years, scientists have studied the area by gravity and magnetic methods (FENG, et al, 1989), geothermal field (WU, et al, 1988; TIAN, ZHANG, 19… 相似文献