全文获取类型
收费全文 | 2368篇 |
免费 | 381篇 |
国内免费 | 711篇 |
专业分类
测绘学 | 12篇 |
大气科学 | 35篇 |
地球物理 | 469篇 |
地质学 | 2203篇 |
海洋学 | 378篇 |
天文学 | 12篇 |
综合类 | 98篇 |
自然地理 | 253篇 |
出版年
2024年 | 15篇 |
2023年 | 37篇 |
2022年 | 77篇 |
2021年 | 63篇 |
2020年 | 97篇 |
2019年 | 64篇 |
2018年 | 72篇 |
2017年 | 73篇 |
2016年 | 93篇 |
2015年 | 76篇 |
2014年 | 110篇 |
2013年 | 159篇 |
2012年 | 128篇 |
2011年 | 116篇 |
2010年 | 131篇 |
2009年 | 150篇 |
2008年 | 160篇 |
2007年 | 182篇 |
2006年 | 142篇 |
2005年 | 137篇 |
2004年 | 148篇 |
2003年 | 122篇 |
2002年 | 107篇 |
2001年 | 92篇 |
2000年 | 119篇 |
1999年 | 104篇 |
1998年 | 97篇 |
1997年 | 93篇 |
1996年 | 95篇 |
1995年 | 89篇 |
1994年 | 48篇 |
1993年 | 49篇 |
1992年 | 49篇 |
1991年 | 28篇 |
1990年 | 28篇 |
1989年 | 23篇 |
1988年 | 24篇 |
1987年 | 17篇 |
1986年 | 9篇 |
1985年 | 10篇 |
1984年 | 7篇 |
1983年 | 8篇 |
1982年 | 5篇 |
1981年 | 2篇 |
1978年 | 2篇 |
1977年 | 2篇 |
1954年 | 1篇 |
排序方式: 共有3460条查询结果,搜索用时 15 毫秒
161.
Kevin Hall 《地球表面变化过程与地形》1982,7(1):45-51
Volcanic activity on sub-Antarctic Marion Island is found to have occurred only during the interglacials. The present volcano distribution is associated with a radial and peripheral fault system, the location of which appears to be related to the former glacier distribution. An hypothesis is presented suggesting that the faulting is a result of deglaciation and that the specific location of the faults is due to the differential stresses occurring between ice-covered and ice-free areas during isostatic uplift. The faulting initiates volcanism due to the location of the island within a volcanic region. 相似文献
162.
Annabel Kelly Richard W. England Peter K. H. Maguire 《Geophysical Journal International》2007,171(3):1172-1184
A regional model of the 3-D variation in seismic P -wave velocity structure in the crust of NW Europe has been compiled from wide-angle reflection/refraction profiles. Along each 2-D profile a velocity–depth function has been digitised at 5 km intervals. These 1-D velocity functions were mapped into three dimensions using ordinary kriging with weights determined to minimise the difference between digitised and interpolated values. An analysis of variograms of the digitised data suggested a radial isotropic weighting scheme was most appropriate. Horizontal dimensions of the model cells are optimised at 40 × 40 km and the vertical dimension at 1 km. The resulting model provides a higher resolution image of the 3-D variation in seismic velocity structure of the UK, Ireland and surrounding areas than existing models. The construction of the model through kriging allows the uncertainty in the velocity structure to be assessed. This uncertainty indicates the high density of data required to confidently interpolate the crustal velocity structure, and shows that for this region the velocity is poorly constrained for large areas away from the input data. 相似文献
163.
Effect of agricultural land use on the chemistry of groundwater from basaltic aquifers, Jeju Island, South Korea 总被引:2,自引:0,他引:2
Dong-Chan Koh Kyung-Seok Ko Yongje Kim Seung-Gu Lee Ho-Wan Chang 《Hydrogeology Journal》2007,15(4):727-743
Geochemical processes were identified as controlling factors of groundwater chemistry, including chemical weathering, salinization from seawater and dry sea-salt deposition, nitrate contamination, and rainfall recharge. These geochemical processes were identified using principal component analysis of major element chemistry of groundwater from basaltic aquifers in Jeju Island, South Korea, a volcanic island with intense agricultural activities. The contribution of the geochemical processes to groundwater chemistry was quantified by a simple mass-balance approach. The geochemical effects due to seawater were considered based on Cl contributions, whereas the effects due to natural chemical weathering were based on alkalinity. Nitrogenous fertilizers, and especially the associated nitrification processes, appear to significantly affect groundwater chemistry. A strong correlation was observed between Na, Mg, Ca, SO4 and Cl, and nitrate concentrations in groundwater. Correspondingly, the total major cations, Cl, and SO4 in groundwater were assessed to estimate relative effect of N-fertilizer use on groundwater chemistry. Cl originates more from nitrate sources than from seawater, whereas SO4 originates mostly from rainwater. N-fertilizer use has shown the greatest effect on groundwater chemistry, particularly when nitrate concentrations exceed 6–7 mg/L NO3–N. Nitrate contamination significantly affects groundwater quality and 18% of groundwater samples have contamination-dominated chemistry. 相似文献
164.
165.
Recent Geochemical Variation of the Hot-Spring Gases from the Tianchi Volcano, Changbai Mountains, Northeast China 总被引:1,自引:0,他引:1
Recent fluid monitoring work shows that the contents of mantle-derived CO_2,He and CH_4 increased anomalously in 2002 and 2003. The 3He/4He ratio of the deep-fault-type Jinjiang hot springs increased highly anomalously in 2003, and then decreased in 2004. The 3He/4He ratio from the thermal-reservoir-type Changbaijulong hot springs increased slowly in 2003, and the increase continued in 2004. The mantle-derived He content of the He released from the Changbaijulong springs increased obviously in 2004. The anomaly of the released gases and the isotopic He was consistent with the trends of seismic activities in the Tianchi volcanic area between 2002 and 2004. The abnormal release of the Jinjiang hot springs apparently decreased after the seismic activities ceased in the second half of 2004, while the abnormal release from the Changbaijulong increased significantly after these seismic activities. It shows that the abnormal release of magmas-derived gases from the thermal-reservoir-type springs lags behind that of the deep-fault-type springs. These characteristics may be of great significance for identifying deep magmatic activity and predicting volcanic earthquakes in the future. 相似文献
166.
Ken Thomson 《Bulletin of Volcanology》2007,70(2):183-201
Three-dimensional seismic data from the Faeroe-Shetland Basin provides detailed information on the relationships between sills,
dykes, laccoliths and contemporaneous volcanic activity. The data shows that sills are predominantly concave upwards, being
complete or partial versions of radially or bilaterally symmetrical forms that possess flat inner saucers connected to a flat
outer rim by a steeply inclined sheet. Such morphologies are only partially modified by pre-existing faults. Sills can be
sourced from dykes or the steep climbing portions of deeper sills. Both sills and dykes can provide magma to overlying volcanic
fissures and sills can be shown to feed shallow laccoliths. Magma flow patterns, as revealed by opacity rendering, suggest
that sills propagate upwards and outwards away from the magma feeder. As an individual sill can consist of several leaves
emplaced at different stratigraphic levels, and as a sill or dyke can provide magma to volcanic fissures, other sills and
laccoliths, the data suggests that neutral buoyancy concepts may not provide a complete explanation for the mechanism and
level of sill emplacement. Instead, the data suggests that the presence of lithological contrasts, particularly ductile horizons
such as overpressured shales may permit sill formation at any level below the neutrally buoyant level.
Electronic supplementary material The online version of this article (doi:) contains supplementary material, which is available to authorized users.
Ken Thomson–deceased, April 2007 相似文献
167.
A new mesh refinement strategy for generating high quality unstructured meshes of the Northwestern European continental shelf, the continental slope and the neighbouring ocean is presented. Our objective is to demonstrate the ability of anisotropic unstructured meshes to adequately address the challenge of simulating the hydrodynamics occurring in these three regions within a unique mesh. The refinement criteria blend several hydrodynamic considerations as the tidal wave propagation on the continental shelf and the hydrostatic consistency condition in steep areas. Several meshes illustrate both the validity and the efficiency of the refinement strategy. The selection of the refinement parameters is discussed. Finally, an attempt is made to take into account tidal ellipses, providing another cause for anisotropy in the mesh. 相似文献
168.
169.
Regional phases in continental and oceanic environments 总被引:1,自引:0,他引:1
170.