全文获取类型
收费全文 | 8494篇 |
免费 | 2195篇 |
国内免费 | 3065篇 |
专业分类
测绘学 | 1366篇 |
大气科学 | 1593篇 |
地球物理 | 1723篇 |
地质学 | 5271篇 |
海洋学 | 1615篇 |
天文学 | 254篇 |
综合类 | 850篇 |
自然地理 | 1082篇 |
出版年
2024年 | 67篇 |
2023年 | 235篇 |
2022年 | 678篇 |
2021年 | 753篇 |
2020年 | 543篇 |
2019年 | 713篇 |
2018年 | 660篇 |
2017年 | 632篇 |
2016年 | 663篇 |
2015年 | 693篇 |
2014年 | 694篇 |
2013年 | 755篇 |
2012年 | 845篇 |
2011年 | 755篇 |
2010年 | 743篇 |
2009年 | 674篇 |
2008年 | 622篇 |
2007年 | 597篇 |
2006年 | 487篇 |
2005年 | 399篇 |
2004年 | 262篇 |
2003年 | 169篇 |
2002年 | 178篇 |
2001年 | 170篇 |
2000年 | 147篇 |
1999年 | 126篇 |
1998年 | 75篇 |
1997年 | 69篇 |
1996年 | 45篇 |
1995年 | 59篇 |
1994年 | 39篇 |
1993年 | 40篇 |
1992年 | 40篇 |
1991年 | 27篇 |
1990年 | 17篇 |
1989年 | 11篇 |
1988年 | 15篇 |
1987年 | 7篇 |
1986年 | 6篇 |
1985年 | 6篇 |
1984年 | 4篇 |
1983年 | 3篇 |
1981年 | 2篇 |
1980年 | 2篇 |
1979年 | 2篇 |
1975年 | 2篇 |
1962年 | 7篇 |
1958年 | 5篇 |
1957年 | 4篇 |
1954年 | 4篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
111.
Two elongatoolithid dinosaur eggs from the Upper Cretaceous of Ganzhou, Jiangxi Province and the embryonic skeletons they bear are described. They represent the first oviraptorosaurian eggs with embryonic skeletons in China and provide the first example that an oospecies can be correlated to certain dinosaur taxon/taxa. The two eggs are the same as the pair of the eggs inside a female oviraptorosaurian pelvis from the same horizon of the same area in both macro- and micro-structures of the egg shells, and can he referred to the oospecies, Macroolithus yaotunensis Zhao, 1975. The morphology of the preserved part of the embryonic skeletons indicates that they may have been laid by an oviraptorid, Heyuannia huangi from Guangdong Province or a closely related oviraptorosaurian, which may have been lived in the Ganzhou area too in the Late Cretaceous. The embryonic skeletons of the two eggs are not in the same developing stage. In one of the eggs, the postzygapophysis of the preserved vertebrae are well ossified, indicating that it was just hatched. 相似文献
112.
Palygorskite is a typical indicator mineral of the arid and strong evaporation environment. Distribution of palygorskite in loess-red clay sequences may act as an important indicator for reconstruction of the paleoenvironment and paleoclimate. In this paper, field emission scanning electron microscope and high-resolution transmission electron microscope observations on the red clay-loess-paleosol of the Renjiapo profile at Lingtai, Gansu Province indicate that palygorskite occurs widely in red clay sequences formed before 3.6 Ma, but no occurrence has been found in eolian sediments since 3.2 Ma. Micromorphological features and microstructure of palygorskite show that it is an autogenic mineral formed during pedogenesis, and transformed from iilite-montmorilionite under the pore water action. In the Lingtai profile, the disappearance horizon of palygorskite is consistent with those of increasing magnetic susceptibility, dust flux and depositional rate. The distribution of palygorskite in the profile indicates that the interval of around 3.6 Ma was an important transformation period of the East Asian paleomonsoon, when changes took place in the East Asia paleoclimate pattern, i.e. a high-frequency strong fluctuation alternative evolution of the environment. Therefore, palygorskite is a key indicator mineral of the East Asian paleomonsoon evolution of that time. 相似文献
113.
Multifractal Analysis of Element Distribution in Skarn-type Deposits in the Shizishan Orefield, Tongling Area, Anhui Province, China 总被引:3,自引:1,他引:2
Wang Qingfei Deng Jun Wan Li Zhao Jie Gong Qingjie Yang Liqiang Zhou Lei Zhang Zhijun 《《地质学报》英文版》2008,82(4):896-905
A series of element concentrations sampled from four drill cores with a length about 1000 m into different skarn-type deposits were selected from the Shizishan orefield, central Tongling, southeastern part of Anhui Province. Using the multifractal method, the distribution and migration characteristics of the major and trace elements are analyzed. The multifractal spectrum of the major elements is left-skewed, whereas the spectrum of the trace elements is right-skewed, which shows that in the process of skarn formation, the trace elements were enriched only locally, and major elements transported within a much larger range. The correlation coefficients of the multifractal parameters Aa (width of the multifractal spectrum) of the four drill cores are relatively low, but the correlation coefficients of the multifractal parameters R (spectrum symmetry parameter) and Af are relatively higher, indicating that although the non-homogeneous intensity of the distribution of elements is inconsistent, their spatial accumulation patterns are almost the same during the ore-forming process. The statistics of the mnltifractal parameters of various elements in the different locations show that the ore-forming processes and element migration pattern in the Shizishan orefield are consistent, and that the migrations of trace elements and major elements exhibit some differences. 相似文献
114.
流变学:构造地质学和地球动力学的支柱学科 总被引:12,自引:6,他引:6
地球是一动态系统,其各层圈的构造运动归根到底就是多矿物复合岩石在各种物理条件(例如,温度、围压、差应力、应变速率、应变方式等)下和化学环境(例如,氧逸度和水含量)中的形变。流变学作为研究岩石力学性质和变形行为的科学,现已成为地球动力学和构造地质学的支柱学科。本文对国际上近年来岩石流变学的最新进展做些扼要的介绍,呼吁中国固体地学界加强流变学的研究,做出经得起时间淘洗、实践检验的原创性成果来,使中国的构造地质学研究迈进国际先进的行列。 相似文献
115.
116.
117.
118.
119.
湖南万古金矿地质地球化学特征及其成因探讨 总被引:3,自引:0,他引:3
万古金矿位于江南古陆金成矿带中段的湘东北金成矿区.地质地球化学研究表明,万古金矿的成矿作用受区域构造控制,NE向断裂断为主要控矿构造,含矿构造是低序次的NWW向扩容断裂构造;成矿物质具有多源性,成矿流体具有岩浆水与变质水的混合水特征.结合区域大地构造背景的分析,认为在中生代中国东部受太平洋板块向西俯冲的影响,形成一系列NE向大断裂,万古金矿的形成与NE向长平大断裂密切相关,携带成矿物质的深部流体沿该断裂上升与浅部残余变质热液混合,并通过淋滤抽提地层中的成矿物质,使流体系统中的成矿物质不断富集,最终在适宜的温压条件下于剪切扩容空间中沉淀成矿. 相似文献
120.