全文获取类型
收费全文 | 721篇 |
免费 | 167篇 |
国内免费 | 101篇 |
专业分类
测绘学 | 47篇 |
大气科学 | 25篇 |
地球物理 | 472篇 |
地质学 | 220篇 |
海洋学 | 95篇 |
天文学 | 10篇 |
综合类 | 28篇 |
自然地理 | 92篇 |
出版年
2024年 | 3篇 |
2023年 | 6篇 |
2022年 | 8篇 |
2021年 | 14篇 |
2020年 | 20篇 |
2019年 | 32篇 |
2018年 | 32篇 |
2017年 | 34篇 |
2016年 | 37篇 |
2015年 | 27篇 |
2014年 | 41篇 |
2013年 | 38篇 |
2012年 | 41篇 |
2011年 | 38篇 |
2010年 | 32篇 |
2009年 | 45篇 |
2008年 | 37篇 |
2007年 | 55篇 |
2006年 | 61篇 |
2005年 | 47篇 |
2004年 | 42篇 |
2003年 | 34篇 |
2002年 | 36篇 |
2001年 | 21篇 |
2000年 | 22篇 |
1999年 | 25篇 |
1998年 | 19篇 |
1997年 | 20篇 |
1996年 | 22篇 |
1995年 | 17篇 |
1994年 | 22篇 |
1993年 | 13篇 |
1992年 | 9篇 |
1991年 | 9篇 |
1990年 | 4篇 |
1989年 | 9篇 |
1988年 | 3篇 |
1987年 | 1篇 |
1986年 | 5篇 |
1985年 | 3篇 |
1981年 | 1篇 |
1980年 | 1篇 |
1979年 | 1篇 |
1954年 | 2篇 |
排序方式: 共有989条查询结果,搜索用时 200 毫秒
81.
IntroductionAfteramoderateorstronger(Ms25.0)earthquake,themosturgentworkofthedivisionforearthquakemonitoringandpredictionistodetermineitstimeoforigin,hypocentrallocation(longitude,latitudeanddepth)andmagnitudeandtojudgethetrendofseismicregimedevelopmentassoonaspossible.Ingeneralcases,whenanearthquakewithMS25.0insideChinaoraonewithMS26.0inneighboringareasofChinahasoccurred,theEarthquakeBulletinofChineseSeismologicalNetworkcanprovidedeterminationoftheorigintime,hypocentrallocation(longitude,… 相似文献
82.
Relationships between moment magnitude and fault parameters: theoretical and semi-empirical relationships 总被引:1,自引:0,他引:1
Fault parameters are important in earthquake hazard analysis. In this paper, theoretical relationships between moment magnitude and fault parameters including subsurface rupture length, downdip rupture width, rupture area, and average slip over the fault surface are deduced based on seismological theory. These theoretical relationships are further simplified by applying similarity conditions and an unique form is established. Then, combining thc simplified theoretical relationships between moment magnitude and fault parameters with seismic source data selected in this study, a practical semi-empirical relationship is established. The seismic source data selected is also to used to derive empirical relationships between moment magnitude and fault parameters by the ordinary least square regression method. Comparisons between semi-empirical relationships and empirical relationships show that the former depict distribution trends of data better than the latter. It is also observed that downdip rupture widths of strike slip faults are saturated when moment magnitude is more than 7.0, but downdip rupture widths of dip slip faults are not saturated in the moment magnitude ranges of this study. 相似文献
83.
生物成因与无机成因文石的FTIR光谱区别 总被引:4,自引:1,他引:4
对16种贝壳交叉页片层中生物成因文石的FT IR谱进行测量,并与无机成因文石进行对比和统计分析后,首次发现生物成因与无机成因文石的FT IR光谱有明显可区分的特征,生物成因文石2ν带(面外弯曲振动)频率平均值为863.4 cm-1,而无机成因文石该带的平均值为855.5 cm-1,两者频率位移达7.9 cm-1。因此文石的2ν带可作为指纹带鉴别生物和无机成因文石。 相似文献
84.
用不变矩从机载激光扫描测高点云数据中重建规则房屋 总被引:4,自引:0,他引:4
介绍了不变矩的概念,结合实例,基于机载激光扫描测高的三雏点云数据,用不变矩实现了规则房屋的模型重建。对不变矩重建房屋模型的精度进行了讨论和分析.得出了一些有益的结论。 相似文献
85.
I. Markiewicz W. G. Strupczewski K. Kochanek V. P. Singh 《Stochastic Environmental Research and Risk Assessment (SERRA)》2006,20(6):391-405
Three dispersion measures of a random variable, i.e., the standard deviation, the mean deviation (MD) about the mean and the second L-moment, are analyzed in terms of their properties and mutual relationships. Emphasis is placed on the MD, as it is less recognized than two other dispersion measures. The relationships between the dispersion measures are derived for distributions commonly applied in flood frequency analysis (FFA). For distributions that are unbounded, there is a distribution-dependent constant value of the ratio of dispersion measures, or equivalently of respective coefficients of variation. For two-parameter distributions that are lower-bounded, the relationship between the coefficients of variation is also distribution dependent and is not linear. For lower-bounded three-parameter distributions, the dispersion measure ratios, or equivalently the ratios of coefficients of variation, depend on the coefficient of skewness and show a strong distributional dependence. For selected distributions, the three dispersion measures are compared both in terms of the robustness to the largest samples element and the accuracy of upper quantile estimation. The MD statistics may be highly competitive to the two other dispersion measure statistics if applied in FFA for parameters estimation. 相似文献
86.
The Harvard CMT catalogue contains 481 shallow earthquakes that occurred between 1 January 1977 and 30 November 2005 within
a broad region defined by the geographical latitude from 3°S to 14°N and by the longitude from 91°E to 102°E. There are 230
events that occurred before the great earthquake of 26 December 2004. Their surface distribution is not uniform and the source
area of the 2004 great event appears as an area of seismic quiescence with a radius of about 100 km. There are 186 events
that occurred between the two great earthquakes of 26 December 2004 and 28 March 2005. Practically all of them are located
to the northwest from the great earthquake of 2005, that in turn was followed by 63 events, mostly located to the southeast.
The cumulative seismic moment from earthquakes before the occurrence of the great event of 2004 increased rather regularly
with time, with sudden increase about twenty years and two years before the occurrence of the great event. The seismic moment
of earthquakes between the two great events increased rapidly during the first ten-fifteen days, then flattened out and increased
slowly with time. After the great event of 2005 the seismic moment shows quiet increase during some 115 days, then sudden
jump, followed by very small activity till the end of our observations. From the spatial distribution of seismic moment of
earthquakes that occurred before the great event of 2004 it follows that its largest release appeared to the southeast from
the great event, around the rupture area of the great earthquake of 2005. The largest release of seismic moment from earthquakes
between the two great events is observed in the vicinity of the 2004 event and further up to the north. The seismic moment
from earthquakes that occurred after the great event of 2005 was mostly released in its vicinity and further down to the south. 相似文献
87.
88.
鲜水河断裂带是四川西部一条晚第四纪强烈左旋走滑活动的构造带,历史上发生多次强震. 它与西北侧的甘孜—玉树断裂带一起,构成青藏高原东部的侧向滑移构造系统中的川滇活动地块的北边界——羌塘地块的东北边界. 鲜水河断裂带北西段可以分成4个段落,每一段落均可作为一个独立的基本破裂单元而发生地震破裂,亦有可能发生不同尺度的多段联合瞧裂. 对鲜水河断裂带北西段不同尺度破裂的震级及复发间隔进行研究. 根据该地区的地质、地球物理、测量及地震等方面的资料,结合我国强震复发的特点,分析了拉分盆地内部的滑动速率分布,以确定各段落的等效长度和倾向宽度,从而建立适合我国大陆走滑断裂的面波震级与断裂发震面积的关系式;进而运用地震矩方法,考虑断层之间的相互作用,结合专家意见建立了该段的矩平衡断裂破裂模型;最后,给出了鲜水河断裂带北西段各破裂源特征化地震的复发间隔、震级大小和不确定性,以及他与中小地震的联合震级分布. 结果表明,鲜水河断裂带北西段较易发生单段破裂,复发间隔在100~150年左右. 相似文献
89.
90.
1994年9月16日台湾海峡7.3级地震震源过程的研究 总被引:1,自引:1,他引:0
采用数字化台网P波波形资料及台湾台网P波初动方向资料,研究了1994年9月16日台湾海峡73级地震及邻近地区(北纬21~26°,东经115~120°)ML≥58级共5次地震的矩张量解及震源参数。结果表明,这次73级地震的矩张量解以双力偶成分为主,是断层面接近NW走向的正断层。断层面的走向与大震前地震的条带分布走向及余震分布显示的破裂图象较相象,震源机制的张应力轴接近水平,近NE走向;压应力轴几乎垂直,近NWW走向,似乎表明这次地震是受菲律海板块向欧亚板块北西向挤压的力源控制。从P轴接近竖直而T轴接近水平来看,发震断层为强烈拉张性正断层,可能还同时存在垂直向上的应力作用。其它4个强震的震源机制解与73级大震的差别较大。这些地震震源机制解的复杂性,表明台湾海峡地震序列的发展过程比较复杂。 相似文献