全文获取类型
收费全文 | 2030篇 |
免费 | 276篇 |
国内免费 | 543篇 |
专业分类
测绘学 | 294篇 |
大气科学 | 109篇 |
地球物理 | 279篇 |
地质学 | 1105篇 |
海洋学 | 307篇 |
天文学 | 28篇 |
综合类 | 224篇 |
自然地理 | 503篇 |
出版年
2024年 | 3篇 |
2023年 | 24篇 |
2022年 | 76篇 |
2021年 | 85篇 |
2020年 | 86篇 |
2019年 | 110篇 |
2018年 | 98篇 |
2017年 | 71篇 |
2016年 | 90篇 |
2015年 | 86篇 |
2014年 | 99篇 |
2013年 | 146篇 |
2012年 | 113篇 |
2011年 | 122篇 |
2010年 | 121篇 |
2009年 | 122篇 |
2008年 | 116篇 |
2007年 | 140篇 |
2006年 | 117篇 |
2005年 | 107篇 |
2004年 | 111篇 |
2003年 | 75篇 |
2002年 | 85篇 |
2001年 | 67篇 |
2000年 | 81篇 |
1999年 | 79篇 |
1998年 | 59篇 |
1997年 | 66篇 |
1996年 | 48篇 |
1995年 | 43篇 |
1994年 | 47篇 |
1993年 | 27篇 |
1992年 | 24篇 |
1991年 | 25篇 |
1990年 | 20篇 |
1989年 | 14篇 |
1988年 | 6篇 |
1987年 | 16篇 |
1986年 | 10篇 |
1985年 | 5篇 |
1984年 | 1篇 |
1983年 | 2篇 |
1981年 | 2篇 |
1979年 | 3篇 |
1972年 | 1篇 |
排序方式: 共有2849条查询结果,搜索用时 343 毫秒
61.
新材料是发展高新技术产业的基础。根据广西的矿产资源优势和在矿物材料方面的研究基础和技术力量,提出了加强工艺矿物学研究,大力发展广西新型矿物材料的研究开发方向,特别提出了超细改性矿物粉体材料、环保矿物材料、节能保温矿物材料、高技术陶瓷材料和合成矿物晶体材料等材料体系中的重点开发方向。 相似文献
62.
63.
考虑了正应力及剪应力联合作用在岩样的端部,而且,在正应力被视为变量,剪应力被视为常量这一特殊条件下,对剪切带的变形特征及剪切带-带外弹性体系统的失稳判据进行了分析.根据剪切虎克定律及梯度塑性理论,提出了剪切带内部弹性应变、塑性应变及总应变的解析式,对上述三种应变进行积分,提出了剪切带错动弹性位移、塑性位移及总位移的解析式.利用压缩虎克定律及几何关系建立了剪切带外弹性体的刚度的表达式.根据刚度理论,建立了剪切带-带外弹性体系统的失稳判据.考虑岩样端面的剪切应力后,在流动剪切应力相同时,剪切带内部的弹性剪切应变(均匀分布)将增加;剪切带内部的塑性剪切应变(不均匀分布)将减小;剪切带的弹性剪切位移(线性分布)将增加;剪切带的塑性剪切位移(非线性分布)将减小;剪切带错动位移要小一些.另外,剪切应力对剪切带-带外弹性体系统的失稳判据没有影响.失稳判据仅和岩石的本构参数、剪切带倾角及结构尺寸有关. 相似文献
64.
Transformation of Residuals to Avoid Artifacts in Geostatistical Modelling with a Trend 总被引:1,自引:0,他引:1
Trend modelling is an important part of natural resource characterization. A common approach to account for a variable with a trend is to decompose it into a relatively smoothly varying trend and a more variable residual component. Then, the residuals are stochastically modelled independent of the trend. This decomposition can result in values outside the plausible range of variability, such as grades below zero or ratios that exceed 1.0. We transform the residuals conditional to the trend component to explicitly remove these complex features prior to geostatistical modelling. Back transformation of the modelled residual values allows the complex relations to be reproduced. A petroleum-related application shows the robustness of the proposed transformation. Furthermore, a mining application shows that when this conditional transformation is applied to the original variable, instead of the residual, simulated values are assured to be nonnegative. 相似文献
65.
Formation and shortening deformation of a back-arc rift basin revealed by deep seismic profiling, central Japan 总被引:1,自引:0,他引:1
Hiroshi Sato Takaya Iwasaki Shinji Kawasaki Yasutaka Ikeda Nobuhisa Matsuta Tetsuya Takeda Naoshi Hirata Taku Kawanaka 《Tectonophysics》2004,388(1-4):47
The northern Fossa Magna (NFM) basin is a Miocene rift system produced in the final stages of the opening of the Sea of Japan. It divides the major structure of Japan into two regions, with north-trending geological structures to the NE of the basin and EW trending structures to the west of the basin. The Itoigawa-Shizuoka Tectonic Line (ISTL) bounds the western part of the northern Fossa Magna and forms an active fault system that displays one of the largest slip rates (4–9 mm/year) in the Japanese islands. Deep seismic reflection and refraction/wide-angle reflection profiling were undertaken in 2002 across the northern part of ISTL in order to delineate structures in the crust, and the deep geometry of the active fault systems. The seismic images are interpreted based on the pattern of reflectors, the surface geology and velocities derived from refraction analysis. The 68-km-long seismic section suggests that the Miocene NFM basin was formed by an east dipping normal fault with a shallow flat segment to 6 km depth and a deeper ramp penetrating to 15 km depth. This low-angle normal fault originated as a comparatively shallow brittle/ductile detachment in a high thermal regime present in the Miocene. The NFM basin was filled by a thick (>6 km) accumulation of sediments. Shortening since the late Neogene is accommodated along NS to NE–SE trending thrust faults that previously accommodated extension and produce fault-related folds on their hanging wall. Based on our balanced geologic cross-section, the total amount of Miocene extension is ca. 42 km and the total amount of late Neogene to Quaternary shortening is ca. 23 km. 相似文献
66.
根据新土地分类在南海区1∶1000土地利用现状调查中的应用,采用文献分析法和实例验证法,探讨其在大比例尺土地利用现状调查中的适用性。结果表明:新土地分类在使用中存在诸如分类层次数目少且略显粗糙以及界线不严谨等问题。提出建议:增加分类层次熏进一步细化分类;更清晰表达地类涵义以及统一分类标准等。 相似文献
67.
Weights of Evidence Modeling of Mineral Potential: A Case Study Using Small Number of Prospects,Abra, Philippines 总被引:9,自引:1,他引:9
Weights of evidence (WofE) modeling usually is applied to map mineral potential in areas with large number of deposits/prospects. In this paper, WofE modeling is applied to a case study area measuring about 920 km2 with 12 known porphyry copper prospects. A pixel size of 100 m × 100 m was used in the spatial data analyses to represent in a raster-based GIS lateral extents of prospects and of geological features considered as spatial evidence. Predictor maps were created based on (a) estimates of studentized values of positive spatial association between prospects and spatial evidence; (b) proportion of number of prospects in zones where spatial evidence is present; and (c) geological interpretations of positive spatial association between prospects and spatial evidence. Uncertainty because of missing geochemical evidence is shown to have an influence on tests of assumption of conditional independence (CI) among predictor maps with respect to prospects. For the final predictive model, assumption of CI is rejected based on omnibus test but is accepted based on a new omnibus test. The final predictive model, which delineates 30% of study area as zones with potential for porphyry copper, has 83% success rate and 73% prediction rate. The results demonstrate plausibility of WofE modeling of mineral potential in large areas with small number of mineral prospects. 相似文献
68.
69.
70.
2002年3月3日大桥水库诱发了Ms4.6级水库地震,其发震构造是安宁河东支断裂近傍具有正断层性质的一个分支断裂。据大桥台网7年多库区地震观测事件记录,地震空间分布上水体附近有一个明显的活跃过程,大坝上游发生小震群,大坝下游发生主震序列。地震的震源深度在蓄水前后有明显变化。4.6级地震的震源机制解的主压应力轴方位和倾角与大多数活动断裂上的地震有明显的差别,主压应力轴的倾角与其它的水库地震相比也存在较大差别。 相似文献