全文获取类型
收费全文 | 354篇 |
免费 | 28篇 |
国内免费 | 2篇 |
专业分类
测绘学 | 10篇 |
大气科学 | 32篇 |
地球物理 | 87篇 |
地质学 | 162篇 |
海洋学 | 22篇 |
天文学 | 53篇 |
自然地理 | 18篇 |
出版年
2024年 | 1篇 |
2023年 | 3篇 |
2022年 | 5篇 |
2021年 | 12篇 |
2020年 | 5篇 |
2019年 | 8篇 |
2018年 | 22篇 |
2017年 | 20篇 |
2016年 | 26篇 |
2015年 | 15篇 |
2014年 | 20篇 |
2013年 | 30篇 |
2012年 | 26篇 |
2011年 | 29篇 |
2010年 | 18篇 |
2009年 | 22篇 |
2008年 | 11篇 |
2007年 | 17篇 |
2006年 | 15篇 |
2005年 | 19篇 |
2004年 | 13篇 |
2003年 | 9篇 |
2002年 | 6篇 |
2001年 | 5篇 |
2000年 | 5篇 |
1998年 | 4篇 |
1997年 | 4篇 |
1996年 | 3篇 |
1992年 | 2篇 |
1991年 | 2篇 |
1989年 | 2篇 |
1988年 | 2篇 |
1951年 | 1篇 |
1950年 | 1篇 |
1949年 | 1篇 |
排序方式: 共有384条查询结果,搜索用时 31 毫秒
301.
302.
303.
304.
Sung Hi Choi Samuel B. Mukasa Alexandre V. Andronikov Maria C. Marcano 《Contributions to Mineralogy and Petrology》2007,153(4):443-463
An origin of the Tinaquillo Peridotite Complex in northern Venezuela, and a model for the tectonic framework of the boundary
zone between the southern Caribbean Plate margin and the South American Plate (SAP) during Late Jurassic to Mid-Cretaceous
time are developed using newly measured Sr, Nd, Pb and Hf isotopic compositions as well as major and trace element geochemistry
for some hornblendite veins and their spinel peridotite host rocks. Depleted geochemical characteristics, principally major
element concentrations, and Nd and Hf isotopes (e.g., εNd = + 27; εHf = +50; ca. 3.4 Ga-Nd model age) of the Tinaquillo peridotites suggest a genetic link between this complex and the Guiana
Shield farther to the south within Venezuela. Scattered zones within the Tinaquillo peridotite were overprinted by what we
interpret as channelized hydrous fluids (<∼3%) derived from the eastward-dipping subduction of the Farallon Plate beneath
the SAP in the Late Jurassic, leading to modification of the original Sr, Nd and Hf isotopic compositions as well as the incompatible
element concentrations. The hornblendite veins have Sr, Nd, Pb and Hf isotopic compositions, falling within the range of present-day
Pacific/Atlantic MORB, but trace element abundance patterns with combinations of arc- and MORB-like characteristics. These
results rule out the possibility of local melting of the host peridotites to produce magmas from which the hornblendite veins
formed. We suggest that during inception of the westward-dipping subduction of the Protocaribbean Plate immediately following
polarity reversal in the Mid-Cretaceous, melts infiltrated the mantle lithosphere and produced the veins. 相似文献
305.
Alexandre Grondeau 《GeoJournal》2007,68(1):31-40
Since the 1990s, information and communication technologies clusters (ICT clusters) have been created in developing countries,
especially in Asia, where India is one of the most dynamic countries. Bangalore and Hyderabad are two important examples of
Indian clusters. This article aims to analyze the characteristics of ICT clusters, Indian policies to develop IC technologies,
the formation and emergence of the Bangalore and Hyderabad clusters and their impacts on the population, as well as to show
that ICT development is a strategic issue for India but does not benefit all of its population. 相似文献
306.
Kenji Yoshikawa Vladimir Romanovsky Nataria Duxbury Jerry Brown Alexandre Tsapin 《冰川冻土》2004,26(Z1):301-309
Direct current resistivity and ground penetrating radar surveys were employed to obtain the value of the resistivity and dielectric constant in the brine near the Barrow, Alaska. The geophysical surveys were undertaken together with the permafrost drilling program for the measuring of the ground temperature regime and for the core sampling. The sampled cores were measured for their physical and chemical properties in the laboratory under different temperature conditions (-60 to 20 ℃). Laboratory results support field observations and led to the development of a technique for distinguishing freshwater taliks and brine layers in permafrost. These methods were also employed in freshwater taliks near Council,Alaska. The electrical resistivity is a powerful and sensitive parameter for brine detection. However, the resistivity is a less sensitive indicator of the soil type or water content under highly saline conditions.High frequency dielectric constant is an ideal second parameter for the indication of the soil type, liquid water content and other physical properties. The imaginary part of the dielectric constant and resistivity have a significant dependence upon salinity, i.e. upon freezing temperature. The ground temperature regime and the freezing point of the brine layer are important parameters for studying the electric properties of permafrost terrain. 相似文献
307.
David Boutelier Alexandre Chemenda Cedric Jorand 《Earth and Planetary Science Letters》2004,222(1):209-216
Thermo-mechanical physical modelling of continental subduction is performed to investigate the exhumation of deeply subducted continental crust. The model consists of two lithospheric plates made of new temperature sensitive analogue materials. The lithosphere is underlain by liquid asthenosphere. The continental lithosphere contains three layers: the weak sedimentary layer, the crust made of a stronger material, and of a still stronger lithospheric mantle. The whole model is subjected to a constant vertical thermal gradient, causing the strength reduction with depth in each lithospheric layer. Subduction is driven by both push force and pull force. During subduction, the subducting lithosphere is heating and the strength of its layers reduces. The weakening continental crust reaches maximal depth of about 120 km and cannot subduct deeper because its frontal part starts to flow up. The subducted crust undergoes complex deformation, including indicated upward ductile flow of the most deeply subducted portions and localised failure of the subducted upper crust at about 50-km depth. This failure results in the formation of the first crustal slice which rises up between the plates under the buoyancy force. This process is accompanied by the delamination of the crustal and mantle layers of the subducting lithosphere. The delamination front propagates upwards into the interplate zone resulting in the formation of two other crustal slices that also rise up between the plates. Average equivalent exhumation rate of the crustal material during delamination is about 1 cm/year. The crust-asthenosphere boundary near the interplate zone is uplifted. The subducted mantle layer then breaks off, removing the pull force and thereby stopping the delamination and increasing horizontal compression of the lithosphere. The latter produces shortening of the formed orogen and the growth of relief. The modelling reveals an interesting burial/exhumation evolution of the sedimentary cover. During initial stages of continental subduction the sediments of the continental margin are dragged to the overriding plate base and are partially accreted at the deep part of the interplate zone (at 60-70 km-depth). These sediments remain there until the beginning of delamination during which the pressure between the subducted crust and the overriding plate increases. This results in squeezing the underplated sediments out. Part of them is extruded upwards along the interplate zone to about 30-km depth at an equivalent rate of 5-10 cm/year. 相似文献
308.
Pieter R. van Oel Eduardo S. P. R. Martins Alexandre C. Costa Niko Wanders Henny A. J. van Lanen 《水文科学杂志》2020,65(Z1):979-990
ABSTRACTTo effectively manage hydrological drought, there is an urgent need to better understand and evaluate its human drivers. Using the “downstreamness” concept, we assess the role of a reservoir network in the emergence and evolution of droughts in a river basin in Brazil. In our case study, the downstreamness concept shows the effect of a network of reservoirs on the spatial distribution of stored surface water volumes over time. We demonstrate that, as a consequence of meteorological drought and recovery, the distribution of stored volumes became spatially skewed towards upstream locations, which affected the duration and magnitude of hydrological drought both upstream (where drought was alleviated) and downstream (where drought was aggravated). The downstreamness concept thus appears to be a useful entry point for spatiotemporally explicit assessments of hydrological drought and for determining the likelihood of progression from meteorological drought to a human-modified hydrological drought in a basin. 相似文献
309.
Chanut Marie-Aurélie Gasc-Barbier Muriel Dubois Laurent Carotte Alexandre 《Landslides》2021,18(9):3101-3118
Landslides - Nowadays, the 3D modelling of surfaces is widely used to provide point clouds in geosciences. To study the evolution of landslides, many point clouds are available but post-processing... 相似文献
310.