全文获取类型
收费全文 | 10968篇 |
免费 | 2663篇 |
国内免费 | 449篇 |
专业分类
测绘学 | 178篇 |
大气科学 | 19篇 |
地球物理 | 10877篇 |
地质学 | 1530篇 |
海洋学 | 98篇 |
天文学 | 11篇 |
综合类 | 947篇 |
自然地理 | 420篇 |
出版年
2024年 | 8篇 |
2023年 | 88篇 |
2022年 | 235篇 |
2021年 | 398篇 |
2020年 | 339篇 |
2019年 | 395篇 |
2018年 | 399篇 |
2017年 | 391篇 |
2016年 | 265篇 |
2015年 | 451篇 |
2014年 | 558篇 |
2013年 | 576篇 |
2012年 | 544篇 |
2011年 | 620篇 |
2010年 | 572篇 |
2009年 | 804篇 |
2008年 | 573篇 |
2007年 | 652篇 |
2006年 | 623篇 |
2005年 | 636篇 |
2004年 | 571篇 |
2003年 | 562篇 |
2002年 | 447篇 |
2001年 | 420篇 |
2000年 | 386篇 |
1999年 | 329篇 |
1998年 | 337篇 |
1997年 | 318篇 |
1996年 | 334篇 |
1995年 | 283篇 |
1994年 | 269篇 |
1993年 | 210篇 |
1992年 | 170篇 |
1991年 | 95篇 |
1990年 | 67篇 |
1989年 | 49篇 |
1988年 | 41篇 |
1987年 | 16篇 |
1986年 | 14篇 |
1985年 | 6篇 |
1984年 | 5篇 |
1983年 | 2篇 |
1979年 | 15篇 |
1978年 | 1篇 |
1977年 | 1篇 |
1954年 | 5篇 |
排序方式: 共有10000条查询结果,搜索用时 78 毫秒
771.
目的,科技进步和社会发展对防震减灾部门提出了更高的工作目标和要求。在未来的一段时期内,一方面需要把地震预报工作从经验基础预报向完善的物理模型推进,另一方面要切实加强地震台网的优化工作,保证研究工作的顺利开展。纵观当前的政治经济形势和地震科学研究现状,文章提出了在“十五”期间应特别关注的几个问题:①正确处理“继承和发展”的关系,努力造就跨世纪的监测预报人才;②监测台网优化和监测技术的发展必须重视预报对监测技术的需求;③分析预报工作的基础建设对提高预报工作质量的作用不容忽视。 相似文献
772.
简要介绍了近年来一些国家地震灾害造成的经济损失占这些国家国内生产总值的比例;主要介绍了多震地区开展地震断层探测研究的概况以断层活动为基础的地震保险试验的内容及研究进展。 相似文献
773.
774.
Takeshi Ohmura Takeo Moriya Chengshi Piao Takaya Iwasaki Toshikastu Yoshi Shin'ichi Sakai Tetsuya Takeda Kaoru Miyashita Humihito Yamazaki Kiyoshi Ito Akira Yamazaki Yoji Shimada Katsuya Tashiro Hiroki Miyamachi 《Island Arc》2001,10(3-4):215-227
Abstract The 1995 Kobe (Hyogo-ken Nanbu) earthquake (MJMA 7.2, Mw 6.9) occurred on Jan. 17, 1995, at a depth of 17 km, beneath the areas of southern part of Hyogo prefecture and Awaji Island. To investigate P-wave velocity distribution and seismological characteristics in the aftershock area of this great earthquake, a wide-angle and refraction seismic exploration was carried out by the Research Group for Explosion Seismology (RGES) . The profile including 6 shot points and 205 observations was 135 km in length, extending from Keihoku, Northern Kyoto prefecture, through Kobe, to Seidan on Awaji Island. The charge of each shot was 350–700 kg. The P-wave velocity structure model showed a complicated sedimentary layer which is shallower than 2.5 km, a 2.5 km-thick basement layer whose velocity is 5.5 km/s, overlying the crystalline upper crust, and the boundary between the upper and lower crust.
Almost all aftershock hypocenters were located in the upper crust. However, the structure model suggests that the hypocenters of the main shock and some aftershock clusters were situated deeper than the boundary between the upper and lower crust. We found that the P-velocity in the upper crust beneath the northern part of Awaji Island is 5.64 km/s which is 3% lower than that of the surrounding area. The low-velocity zone coincides with the region where the high stress moment release was observed. 相似文献
Almost all aftershock hypocenters were located in the upper crust. However, the structure model suggests that the hypocenters of the main shock and some aftershock clusters were situated deeper than the boundary between the upper and lower crust. We found that the P-velocity in the upper crust beneath the northern part of Awaji Island is 5.64 km/s which is 3% lower than that of the surrounding area. The low-velocity zone coincides with the region where the high stress moment release was observed. 相似文献
775.
Quaternary vertical offset and average slip rate of the Nojima Fault on Awaji Island, Japan 总被引:5,自引:0,他引:5
Abstract Drilling was carried out to penetrate the Nojima Fault where the surface rupture occurred associated with the 1995 Hyogo-ken Nanbu earthquake. Two 500 m boreholes were successfully drilled through the fault zone at a depth of 389.4 m. The drilling data show that the relative uplift of the south-east side of the Nojima Fault (south-west segment) was approximately 230 m. The Nojima branch fault, which branches from the Nojima Fault, is inferred to extend to the Asano Fault. From the structural contour map of basal unconformity of the Kobe Group, the vertical component of displacement of the Nojima branch–Asano Fault is estimated to be 260–310 m. Because the vertical component of displacement on the Nojima Fault of the north-east segment is a total of those of the Nojima Fault of the south-west segment and of the Nojima branch–Asano Fault, it is estimated to total to 490–540 m. From this, the average vertical component of the slip rate on the Nojima Fault is estimated to be 0.4–0.45 m/103 years for the past 1.2 million years. 相似文献
776.
Abstract Crack-filling clays and weathered cracks were observed in the Disaster Prevention Research Institute, Kyoto University (DPRI) 1800 m cores drilled from the Nojima Fault Zone, which was activated during the 1995 Hyogo-ken Nanbu earthquake (Kobe earthquake). The crack-filling clays consist mainly of unconsolidated fine-grained materials that fill opening cracks with no shear textures. Most of the cracks observed in the DPRI 1800 m cores are yellow-brown to brown in color due to weathering. Powder X-ray diffraction analyses show that the crack-filling clays are composed mainly of clay minerals and carbonates such as siderite and calcite. Given that the top of the borehole is approximately 45 m above sea level, most of the core is far below the stable groundwater table. Hence, it is suggested that the crack-filling clays and weathered cracks in the cores taken at depths of 1800 m were formed by the flow of surface water down to the deep fractured zone of the Nojima Fault Zone during seismic faulting. 相似文献
777.
778.
Anisotropy of the apparent resistivity variation rate near the epicentral region for strong earthquakes 总被引:1,自引:0,他引:1
IntroductionThe geo-electrical anisotropy before earthquake is of special significance for the prediction of earthquake location and for the research on crustal stress status near the epicentral region. The anisotropy has been studied from various aspects (CHEN, et al, 1983; QIAN, et al, 1985, 1996; LU, et al, 1990a; MAO, et al, 1995; RUAN, et al, 1999). But the anisotropic phenomena presented by geo-electrical data are not practically satisfactory and not clear as compared with the res… 相似文献
779.
根据地震活动特征、大武地震台尾波持续时间及长宁、湟源和西宁 3个台水氡异常变化 ,讨论了 1 999年河南MS5 .1和玛沁MS5 .0地震发生后库玛断裂带的地震活动趋势 .结果表明 ,河南—玛沁地区的中强地震活动与库玛断裂带上的强震活动有明显的对应关系 ;在库玛断裂带中东段存在一个由ML ≥ 3.0地震围成的空区 ;上述2次地震发生后大武地震台尾波持续时间异常依然存在 ,长宁、湟源和西宁台水氡趋势异常仍然持续 .据此认为库玛断裂带存在发生强震的背景 相似文献
780.