全文获取类型
收费全文 | 2522篇 |
免费 | 358篇 |
国内免费 | 521篇 |
专业分类
测绘学 | 96篇 |
大气科学 | 248篇 |
地球物理 | 339篇 |
地质学 | 1565篇 |
海洋学 | 360篇 |
天文学 | 41篇 |
综合类 | 126篇 |
自然地理 | 626篇 |
出版年
2024年 | 8篇 |
2023年 | 32篇 |
2022年 | 67篇 |
2021年 | 97篇 |
2020年 | 104篇 |
2019年 | 116篇 |
2018年 | 114篇 |
2017年 | 99篇 |
2016年 | 116篇 |
2015年 | 126篇 |
2014年 | 134篇 |
2013年 | 216篇 |
2012年 | 127篇 |
2011年 | 159篇 |
2010年 | 126篇 |
2009年 | 150篇 |
2008年 | 176篇 |
2007年 | 149篇 |
2006年 | 172篇 |
2005年 | 149篇 |
2004年 | 153篇 |
2003年 | 131篇 |
2002年 | 116篇 |
2001年 | 70篇 |
2000年 | 76篇 |
1999年 | 89篇 |
1998年 | 43篇 |
1997年 | 53篇 |
1996年 | 37篇 |
1995年 | 40篇 |
1994年 | 41篇 |
1993年 | 24篇 |
1992年 | 7篇 |
1991年 | 21篇 |
1990年 | 12篇 |
1989年 | 7篇 |
1988年 | 3篇 |
1987年 | 7篇 |
1986年 | 8篇 |
1985年 | 7篇 |
1984年 | 5篇 |
1983年 | 4篇 |
1982年 | 4篇 |
1978年 | 1篇 |
1977年 | 4篇 |
1973年 | 1篇 |
排序方式: 共有3401条查询结果,搜索用时 15 毫秒
991.
南天山托云盆地晚白垩世——早第三纪玄武岩的地球化学特征 … 总被引:18,自引:0,他引:18
托云盆地晚白垩世--早第三纪碱性橄榄玄武岩Sr、Nd、Pb同位素组成表明,本区玄武岩以低Sr、Pb和相对高的Nd同位素值(^87Sr/^86Sr为0.703554 ̄0.703884;^143Nd/^144Nd为0.512838 ̄0.512904;^206Pb/^204Pb为18.0063 ̄18.4720;^207Pb/^204Pb为15.4411 ̄15.5060;^208Pb/^204Pb为37. 相似文献
992.
Cobalt Deposits in the Central China Orogenic Belt 总被引:2,自引:0,他引:2
XU Yong Bureau of Geology Exploration B Fuxing Rd. Beijing and ZHU Xinyou Beijing Institute of Geology for Mineral Resources Anwai Beiyuan Beijing 《《地质学报》英文版》2000,74(3):540-543
Cobalt mostly occurs as an associated metal in Cu-Ni sulphide deposits, skarn Fe-Cu-Pb-Zn deposits and volcanic-hosted massive sulphide (VHMS) or sedex deposits. There are different types of cobalt deposits in the Central China orogenic belt. In the Tamu-Kalangu Mississippi-valley type Pb-Zn deposits, many cobalt-nickel sulphide minerals were found. The cobalt content of the ore is 0.064%-0.46% in sedex-type Kendekeke Fe-Pb-Zn-Au deposits, and cobalt sulphide veins with Co contents of 4%-9% have also been found. About 28000 tons of cobalt reserves were delineated in the Dur'ngoi Cu-Co-Zn deposit of VHMS type in the A'nyemaqen Mountains. It is considered that the exploration potential for cobalt is attractive in this district, especially in sedex-type deposits and Co-rich sulphide veins in sedex-type Fe, Cu and Pb-Zn deposits and their surroundings. 相似文献
993.
华北地台沉积岩型金矿床的找矿勘查意义 总被引:1,自引:0,他引:1
冀东地区沉积岩型金矿床主要赋存在中上元古界长城系和蓟县系巨厚钙-镁碳酸盐岩内,金矿化受层间角砾岩带控制。相比之下,内蒙古中西部沉积岩型金矿床主要产出在上元古界青白不钙质粉砂岩和板岩内,矿父母产状受层间构造破碎带控制。尽管上述金矿床的成矿环境、赋矿围岩和成矿时代存在一定差别,但是它们均以埋藏浅、规模大、物质组分简单和易选冶为特点。为突出这两类金矿床的区域性特征,前者命为“长城式”,后者则确定为“阿拉 相似文献
994.
黔中瀑布水生苔藓植物区系及其生物喀斯特沉积生态类型研究 总被引:7,自引:3,他引:4
对贵州中部18个喀斯特瀑布水生苔藓植物进行了研究。瀑布苔藓植物区系种类由14 科23 属38 种组成, 藓类( Mosses) 含8 科17 属31 种, 苔类( Liv erw o rts) 5科5属6种,而角苔类( Ho rnwo r t)仅1科1属1种。区系地理成分含世界分布( 15. 79% ) , 北温带分布( 36. 84% ) ,旧世界温带分布( 5. 26% )、泛热带分布( 2. 63% )、热带亚洲分布( 5. 267% ) , 东亚分布( 26. 32% ) 和中国特有( 7. 90% )等7种成分。根据喀斯特瀑布沉积环境和苔藓植物优势种类组成特征,可划分黔中瀑布苔藓沉积生态类型为溪流瀑布沉积、河流瀑布沉积、石灰华坝沉积和瀑布洞穴沉积4种类型及15种生物喀斯特沉积亚类型。 相似文献
995.
中国南方岩溶区土地石漠化的成因与过程 总被引:18,自引:2,他引:16
中国南方岩溶区是石漠化广为发展的脆弱生态区域。南方岩溶区土地石漠化的起因既有自然因素,也有人为因素。在地质历史时期其自身环境孕育和存在着自然石漠化过程,在历史时期—现代自然石漠化过程又叠加了人为石漠化过程,人为活动加速、加剧了石漠化的发展。清朝初、中期是人为活动影响石漠化的重要转折时期,此后人为因素作用比重逐渐超过自然因素的作用比重。岩溶区土地石漠化过程是由植被退化丧失过程、土壤侵蚀过程、地表水流失过程、基岩溶蚀侵蚀过程、土地生物生产力退化过程合成的地表生态过程,其实质是形成石质荒漠的土地退化过程。 相似文献
996.
997.
The passage of subtropical cold fronts through central Australia produces the only significant mesoscale meteorological features in the region. The interaction of these cold fronts with the surface energy balance strongly affects the local weather and climate. The surface energy balance was measured at a semi-arid site in Alice Springs, central Australia, to determine how it was influenced by the passage of subtropical cold fronts. Both Bowen ratio and eddy correlation methods were used. The daytime energy balance of the site showed high net radiation that was partitioned into 75% sensible heat flux and 25% soil heat flux with little or no latent heat flux. At night there was a large net radiative loss that was balanced primarily by a loss of heat from the soil. The cold fronts predominately passed through Alice Springs at night and showed a strong surface signature. The fronts brought moister air resulting in higher water vapour pressures during their passage. The nocturnal boundary layer was often disturbed as the front passed, resulting in warm, moist air being mixed down toward the land surface. Mixing decreased the soil heat flux and increased latent heat fluxes toward the surface. Moisture that accumulated at the surface at these times was often evaporated after a return to drier conditions. During the daytime, surface signatures in soil and sensible heat fluxes were less distinct due to the strong convective mixing. Latent heat fluxes followed a similar trend to the nocturnal case. 相似文献
998.
Any mine planning requires careful prediction of both the head grade andtonnage ofmineralization. There are various methods of interpolation that attempt to provide reasonable estimatesat unsampled locations. All of these give realizations that are unduly smooth and extremevalues that occur in reality are not reflected in these estimates. Such methods, therefore,provide limited scope for accurate risk assessment. An alternative approach that is rapidlygaining popularity is the method of conditional simulation. This approach attempts to reproduceboth the grade distributions of the sample data as well as its spatial variability. In this paper,a case study is presented on a platinum mineralization to demonstrate and compare sequentialGaussian and sequential conditional simulation techniques and to quantify and discuss therelevant sensitivities. 相似文献
999.
Abstract. To evaluate the effects of beach morphodynamics upon the abundance, tidal movement, population structure and burrowing rate of the crab Emerita analoga (Stimpson) (Anomura, Hippidae) we sampled two beaches in south central Chile (ca. 42° S), Mar Brava and Ahui with dissipative and reflective characteristics, respectively. The swash zone at the dissipative beach was 5 – 6 times wider than that of the reflective beach. A at the dissipative beach, upwash speeds were higher and the number of effluent line crossings were lower by more than an order of magnitude. To examine the tidal movement of E. analoga, we collected crabs from 5 to 6 tidal levels of each beach every 2 h across 12 h of the tidal cycle. The intertidal distribution of crabs differed between beaches; i. e., at the dissipative beach they were primarily located at the swash zone, while at the reflective beach they were mostly located at the low tide level and shallow subtidal. The change in position of crabs was pronounced across the tidal cycle at the dissipative beach (Mar Brava), with most of the animals remaining in the active swash zone. Body size data were used to construct size frequency distributions for each population. Crabs from the dissipative beach reached larger sizes than those at the reflective beach. Sediments were coarser at the latter versus the former beach. Crabs burrowed at similar rates in the sand from both beaches, a result which supports the idea that E. analoga is a “sediment generalist” capable of burrowing successfully in a wide range of sediment types. This characteristic is likely a key to the broad success of this species on the full range of beach morphodynamic types along the coasts of South and North America. 相似文献
1000.
在“等级式成团”(hierarchical clustering)宇宙学演化框架下,早型星系(E/SO)的形成和演化不是如经典的“整体塌缩”(monolithic collapse)演化模式所描述的是由高红移处的短时间剧烈恒星形成过程一次性完成的;相反,它们可能是在大尺度结构形成过程中由盘星系间的相互合并演化而来,特别是对于质量相当的盘星系间的剧烈合并过程。目前的数值模拟和高分辨成像观测都已证实了这种可能性,而且红移巡天的结果也更多地支持这种演化模式。在此提出一个星系合并过程中核区星暴和中心黑洞共生演化的模型,来解释由空间望远镜(HST)和地面CCD高分辨测光所得的早型星系“黑洞/核球”统计线性相关,也即中心黑洞质量约为其核球体质量的0.6%;同时,该演化模型还可以进一步合理地解释在类星体的近红外成像观测中统计得出的相似的线性相关性,即类星体中心亮度与其母星系质量成正比。并给出此模型计算的极限情况和模型的解析估计。 相似文献