全文获取类型
收费全文 | 954篇 |
免费 | 142篇 |
国内免费 | 43篇 |
专业分类
测绘学 | 2篇 |
大气科学 | 41篇 |
地球物理 | 918篇 |
地质学 | 59篇 |
海洋学 | 9篇 |
天文学 | 2篇 |
综合类 | 98篇 |
自然地理 | 10篇 |
出版年
2024年 | 1篇 |
2023年 | 1篇 |
2022年 | 8篇 |
2021年 | 9篇 |
2020年 | 12篇 |
2019年 | 13篇 |
2018年 | 22篇 |
2017年 | 25篇 |
2016年 | 17篇 |
2015年 | 29篇 |
2014年 | 26篇 |
2013年 | 30篇 |
2012年 | 31篇 |
2011年 | 24篇 |
2010年 | 33篇 |
2009年 | 59篇 |
2008年 | 29篇 |
2007年 | 48篇 |
2006年 | 47篇 |
2005年 | 27篇 |
2004年 | 55篇 |
2003年 | 43篇 |
2002年 | 55篇 |
2001年 | 43篇 |
2000年 | 53篇 |
1999年 | 48篇 |
1998年 | 61篇 |
1997年 | 49篇 |
1996年 | 79篇 |
1995年 | 53篇 |
1994年 | 29篇 |
1993年 | 24篇 |
1992年 | 18篇 |
1991年 | 9篇 |
1990年 | 4篇 |
1989年 | 7篇 |
1988年 | 13篇 |
1986年 | 2篇 |
1985年 | 1篇 |
1984年 | 1篇 |
1979年 | 1篇 |
排序方式: 共有1139条查询结果,搜索用时 15 毫秒
991.
地震前兆研究的某些新进展 总被引:1,自引:0,他引:1
本文简要介绍了当前国际上在地震前兆研究方面取得的某些新进展。所介绍的前兆类别包括测震学前兆中的地震活动时空强分布特征、地震活动波与形变波、地震波特征量、高频地脉动、慢地震与“前兆波”,以及非测震学前兆中的应力与应变、地磁场与宇宙辐射、臭氧、重力脉冲、天体运动与电离层等。 相似文献
992.
探讨了北部湾地震地磁和气象的异常现象,初步结果表明,震前几个月至数天,地磁垂直分量的相关系数r值,特征线斜率K值以及Z日变形态双低点位移先后出现短临异常,气象因子分析结果表明,年雨量一阶差分大于400mm可作为5级以上地震的年度预报参考指标。震前数月,-3.2m的地温年变形态出现畸变。 相似文献
993.
Theoretical mean wave resistance and regional division of the energy of single-layer flow over topogra-phy is studied at the near-resonant region in the weakly nonlinear, long wave limit. The theoretical meanwave resistance is determined in terms of the 1st and 2nd conservation laws of the fKdV equation. It isproved by the asymptotic mean method that the theoretical mean wave resistance depends only on the intensityand moving velocity of the topography. The theoretical results of this paper are in good agreement withnumerical calculations. Comparisons between the theoretical and numerical results showed that the theoryof the present paper holds for any small compact topography. 相似文献
994.
本文分析了1989年11月2日宁夏固原5.3级地震前后的地震活动,井分析了其序列特征,判定此震为孤立型地震。本文最后介绍了几起震前认识到的前兆观测资料异常现象。 相似文献
995.
Hartmut Spetzler Guennadi Sobolev Anatoli Koltsov Arno Zang Ivan C. Getting 《Pure and Applied Geophysics》1991,137(1-2):95-112
In this paper we report results obtained from various friction experiments under direct and oblique shear loading conditions. We used four rock types of varying brittleness (quartzite, anhydrite, limestone, pyrophyllite) with different surface roughness. The observations concentrate on the time span several milliseconds before dynamic failure occurs. During this period a premonitory, unstable phase of slip (slip 2) occurs. This differs importantly from a premonitory, stable process (slip 1) with durations of hundreds of seconds. On smooth surfaces slip 2 is usually observed with ductile rocks and less reliably with brittle rocks. Slip 2 is mostly accompanied by acoustic emissions, which increase in rate of occurrence and in magnitude until the stick-slip event. Foreshocks are observed during approximately 50% of the slip 2 events on rough surfaces. Foreshocks far exceed the acoustic noise level, which is also prevalent before stick-slip events on rough surfaces. In the direct shear experiment, where two faults are being loaded simultaneously, in about 20% of the cases precursory slip 2 was observed on the opposite side on which the final stick-slip event occurred. 相似文献
996.
Areas of low strain rate are typically characterized by low to moderate seismicity. The earthquake catalogs for these regions
do not usually include large earthquakes because of their long recurrence periods. In cases where the recurrence period of
large earthquakes is much longer than the catalog time span, probabilistic seismic hazard is underestimated. The information
provided by geological and paleo-seismological studies can potentially improve seismic hazard estimation through renewal models,
which assume characteristic earthquakes. In this work, we compare the differences produced when active faults in the northwestern
margin of the València trough are introduced in hazard analysis. The differences between the models demonstrate that the introduction
of faults in zones characterized by low seismic activity can give rise to significant changes in the hazard values and location.
The earthquake and fault seismic parameters (recurrence interval, segmentation or fault length that controls the maximum magnitude
earthquake and time elapsed since the last event or Te) were studied to ascertain their effect on the final hazard results. The most critical parameter is the recurrence interval,
where shorter recurrences produce higher hazard values. The next most important parameter is the fault segmentation. Higher
hazard values are obtained when the fault has segments capable of producing big earthquakes. Finally, the least critical parameter
is the time elapsed since the last event (Te), when longer Te produces higher hazard values. 相似文献
997.
Wang Yanzhao 《中国地震研究》2007,21(4):355-364
Seismological and geodetic observations indicate that slow slip sometimes occurs in active fault zones beneath the seismogenic depth, and large slow slip can result in transient ground motion. Slow earthquakes, on the other hand, emit tremor-like signals within a narrow frequency band, and usually produce no catastrophic consequences. In general, slow slip and slow earthquakes probably correspond to deformation processes associated with releasing elastic energy in fault zones, and understanding their mechanisms may help improve our understanding of fault zone dynamic processes. This article reviews the research progress on slow slip and slow earthquakes over the last decade. Crustal motion and tremor activities associated with slow slip and slow earthquakes have been investigated extensively, mainly involving locating sources of slow slip and slow earthquakes and numerical modeling of their processes. In the meantime, debates have continued about slow slip and slow earthquakes, such as their origins, relationship, and mechanisms. 相似文献
998.
999.
1000.
地震前兆数据库软件的使用 总被引:2,自引:0,他引:2
新疆地震前兆台网中心通过远程拨号的方式采集各台点的数字化数据,运用前兆通讯、数据服务等软件实现数据的格式转换、入库及基本数据查询等前兆数据库的各种操作,方便了分析人员的使用。初步建立起地震前兆数据库。 相似文献