全文获取类型
收费全文 | 1253篇 |
免费 | 190篇 |
国内免费 | 257篇 |
专业分类
测绘学 | 102篇 |
大气科学 | 235篇 |
地球物理 | 291篇 |
地质学 | 560篇 |
海洋学 | 200篇 |
天文学 | 86篇 |
综合类 | 119篇 |
自然地理 | 107篇 |
出版年
2024年 | 5篇 |
2023年 | 20篇 |
2022年 | 32篇 |
2021年 | 47篇 |
2020年 | 31篇 |
2019年 | 34篇 |
2018年 | 57篇 |
2017年 | 51篇 |
2016年 | 55篇 |
2015年 | 68篇 |
2014年 | 73篇 |
2013年 | 68篇 |
2012年 | 52篇 |
2011年 | 80篇 |
2010年 | 72篇 |
2009年 | 70篇 |
2008年 | 51篇 |
2007年 | 53篇 |
2006年 | 65篇 |
2005年 | 54篇 |
2004年 | 55篇 |
2003年 | 50篇 |
2002年 | 70篇 |
2001年 | 89篇 |
2000年 | 48篇 |
1999年 | 58篇 |
1998年 | 37篇 |
1997年 | 32篇 |
1996年 | 35篇 |
1995年 | 34篇 |
1994年 | 37篇 |
1993年 | 21篇 |
1992年 | 18篇 |
1991年 | 13篇 |
1990年 | 18篇 |
1989年 | 7篇 |
1988年 | 10篇 |
1987年 | 10篇 |
1985年 | 5篇 |
1984年 | 1篇 |
1983年 | 3篇 |
1982年 | 1篇 |
1981年 | 1篇 |
1978年 | 2篇 |
1976年 | 2篇 |
1975年 | 2篇 |
1974年 | 2篇 |
1964年 | 1篇 |
排序方式: 共有1700条查询结果,搜索用时 31 毫秒
41.
福建省水系沉积物微量元素含量特征及成矿远景预测 总被引:6,自引:0,他引:6
根据区域化探水系沉积物测量分析3万余件样品中40种元素含量,统计了32种微量元素的背景平均值,浓度克拉克值,总体变化系数等参数。在利用水系沉积物富集系数估计值对浓度克拉克值进行校正后,使用顺序号累加法对福建省32种元素内生成矿作用的规模进行预测排序,并分析了银,硼的资源潜力。 相似文献
42.
43.
44.
本文介绍了瑶沟等地区勘查金矿的放射性和非放射性气体地球化学方法的研究成果:基本查明了应用本方法勘查金矿的主要条件是金矿中伴生有足够的U,Hg和碳酸盐矿物;研制成了壤中气(Rn-CO2)联测技术,提高了测量质量和探测深部矿体的能力;利用壤中气(Rn-CO2)异常进行了成矿预测,并已获得成功。 相似文献
45.
图像配准和融合及其在医学影像中的应用 总被引:2,自引:2,他引:2
图像配准和融合是图像分析和处理的基本问题,在医学影像、遥感、计算机视觉等领域有着广泛的应用。本文研究它们在多模态医学影像技术中的应用。本文提出并实现了基于Fourier变换的图像配准和基于子波变换的图像融合方法,在图像融合中,我们采用特征选择的取大原则,这种准则更适合于来自不同图像中的明显特征 相似文献
46.
川西甘孜州旅游观光资源丰富多彩,遍布的温泉、热泉与雪山、草地、森林相配置成的景点、景区比比皆是.加之悠久的人文、宗教建筑和文物,都具有很高的研究和观赏价值。开发这些资源以引导甘孜州经济的发展,将是大有可为的。 相似文献
47.
48.
The structures of sodium silicate and aluminosilicate glasses quenched from melts at high pressure (6-10 GPa) with varying degrees of polymerization (fractions of nonbridging oxygen) were explored using solid-state NMR [17O and 27Al triple-quantum magic-angle spinning (3QMAS) NMR]. The bond connectivity in melts among four and highly coordinated network polyhedra, such as [4]Al, [5,6]Al, [4]Si, and [5,6]Si, at high pressure is shown to be significantly different from that at ambient pressure. In particular, in the silicate and aluminosilicate melts, the proportion of nonbridging oxygen (NBO) generally decreases with increasing pressure, leading to the formation of new oxygen clusters that include 5- and 6-coordinated Si and Al in addition to 4-coordinated Al and Si, such as [4]Si-O-[5,6]Si, [4]Si-O-[5,6]Al and Na-O-[5,6]Si. While the fractions of [5,6]Al increase with pressure, the magnitude of this increase diminishes with increasing degrees of ambient-pressure polymerization under isobaric conditions. Incorporating the above structural information into models of melt properties reproduces the anomalous pressure-dependence of O2− diffusivity and viscosity often observed in silicate melts. 相似文献
49.
SuoShutian ZhongZengqiu ZhouHanwen YouZhendong 《中国地质大学学报(英文版)》2004,15(3):262-274
New structural and petrological data unveil a very complicated ductile deformation history of the Xiongdian-Suhe HP metamorphic unit, north-western Dabie Shun, central China. The finegrained symplectic amphibolite-facies assemblage and coronal structure enveloping eclogite-facies garnet,omphacite and phengite etc., representing strain-free decompression and retrogressive metamorphism,are considered as the main criteria to distinguish between the early-stage deformation under HP metamorphic conditions related to the continental deep subduction and collision, and the late-stage deformation under amphibolite to greenschist-facies conditions occurred in the post-eclogite exhumation processes.Two late-stages of widely developed, sequential ductile deformations D3 and D4, are recognized on the basis of penetrative fabrics and mineral aggregates in the Xiongdian-Suhe HP metamorphic unit, which shows clear, regionally, consistent overprinting relationships. D3 fabrics are best preserved in the Suhe tract of low post-D3 deformation intensity and characterized by steeply dipping layered mylonitic amphibolites associated with doubly vergent folds. They are attributed to a phase of tectonism linked to the initial exhumation of the HP rocks and involved crustal shortening with the development of upright structures and the widespread emplacement of garnet-bearing granites and felsic dikes. D4 structures are attributed to the main episode of ductile extension (D^24) with a gently dipping foliation to the north and common intrafolial, recumbent folds in the Xiongdian tract, followed by normal sense top-to-the northductile shearing (D^24) along an important tectonic boundary, the so-called Majiawa-Hexiwan fault (MHF), the westward continuation of the Balifan-Mozitan-Xiaotian fault (BMXF) of the northern Dabie Shan. It is indicated that the two stages of ductile deformation observed in the Xiongdian-Suhe HP metamorphic unit, reflecting the post-eclogite compressional or extrusion wedge formation, the subhorizontal ductile extension and crustal thinning as well as the top-to-the north shearing along the high-angle ductile shear zones responsible for exhumation of the HP unit as a coherent slab, are consistent with those recognized in the Dabie-Sulu UHP and HP metamorphic belts, suggesting that they were closely associated in time and space. The Xiongdian-Suhe HP metamorphic unit thus forms part of the Triassic(250-230 Ma) collision orogenic belt, and can not connect with the South Altun-North Qaidam-North Qinline UHP metamorphic belt formed durin~ the Early Paleozoic (500-400Ma). 相似文献
50.
Self-affinity dimensions of topography and its implications in morphotectonics: an example from Taiwan 总被引:1,自引:0,他引:1
This paper discusses the self-affinity dimensions of landscape surfaces at a short-range scale and the link to morphotectonic features of the young orogenic belts of Taiwan. The variogram method is adopted to estimate such parameters as the fractal dimension (D), the ordinate-intercept (γ) and the range (R) from data subsets of the digital elevation model (DEM) in a moving-window operation. The fractal morphology expressed by D and γ is found to be useful in defining geomorphic provinces that are related to tectonic features. The mountainous terrain is characterized by high gamma values and low fractal dimensions in contrast to the coastal plains where low gamma values and high fractal dimensions are found. A zone, defined by the fractal parameters (2.4<D<2.6 and 0<γ<2.4), is found to coincide with the most tectonically active zone of Taiwan. Active faults often occur at the boundary between landscapes with contrasting fractal patterns. In the flat lowlands along the western coast, the fractal morphology displays a west-facing amphitheatric pattern, which may be related to the indentation of the pre-Miocene Peikang Basement High. The fractal morphology may reflect some subtle changes in surface textures of a landscape sculpted by surface processes, which in turn are influenced by tectonic activities. The surface roughening and diffusive smoothing may concur to shape the landscape surface at the short ranges we discuss in this study. 相似文献