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301.
Morteza Khalatbari-Jafari Thierry Juteau Hervé Bellon Hashem Emami 《Comptes Rendus Geoscience》2003,335(12):917-929
New field and laboratory studies on the ophiolite of Khoy (northwestern corner of Iran) lead to the discovery that there are not one, but two ophiolitic complexes in the Khoy area: (1) an old, poly-metamorphic ophiolite, whose oldest metamorphic amphiboles yielded a Lower Jurassic apparent 40K–40Ar age, and whose primary magmatic age should logically be pre-Jurassic (Upper-Triassic?); (2) a younger non metamorphic ophiolite of well dated Upper Cretaceous age. To cite this article: M. Khalatbari-Jafari et al., C. R. Geoscience 335 (2003). 相似文献
302.
Relationship between point rainfall, average sampled rainfall and ground truth at the event scale in the Sahel 总被引:2,自引:0,他引:2
Abou Amani Thierry Lebel 《Stochastic Environmental Research and Risk Assessment (SERRA)》1998,12(2):141-154
Geostatistical techniques are used to quantify the reference mean areal rainfall (ground truth) from sparse raingaugenetworks.
Based on the EPSAT-Niger event cumulative rainfall, a linear relationship between the ground truth considered as the mean
area rainfall estimated from the densely available raingauge network and the area rainfall estimated from sparse network are
derived. Also, a linear relationship between the ground truth and point rainfall is established. As it was reported experimentally
by some authors, the slope of these relationships is less than one. Based on the geostatistical framework, the slope and the
ordinate at the origin can be estimated as a function of the spatial structure of the rainfall process. It is shown that the
slope is smaller than one. For the special case of one gauge inside a fixed area or a Field Of View (FOV), an areal reduction
factor is derived. It has a limit value which depends only on the size of the area and the spatial structure of the rainfall
process. The relative variance error of estimating the FOV cumulative rainfall from point rainfall is also given. 相似文献
303.
304.
Emmanuelle Ducassou Thierry Mulder Sbastien Migeon Eliane Gonthier Anne Murat Marie Revel Lucilla Capotondi Stefano M. Bernasconi Jean Mascle Sbastien Zaragosi 《Quaternary Research》2008,70(3):382-391
Clastic mud beds rich in continental organic matter are observed recurrently in the Nile deep-sea turbidite system. They formed during flooding periods of the river similar to those that induce sapropel formation and occurred during periods of increased density stratification of the eastern Mediterranean. The very fine-grained flood deposits are intercalated within pelagic sediments, sapropels and Bouma-type turbidites. These flood deposits form by the successive reconcentrations of surface (hypopycnal) plumes by convective sedimentation, which in turn generate a fine-grained low-energy hyperpycnal flow. Sea-level high stands seem also to favor hypopycnal plume formation and increase clastic mud bed formation. Consequently, these muddy clastic beds provide a direct link between deep-marine sedimentary records and continental climatic change through flood frequency and magnitude. 相似文献
305.
William L. Bandy Franois Michaud Jrme Dyment Carlos A. Mortera-Gutirrez Jacques Bourgois Thierry Calmus Marc Sosson Jose Ortega-Ramirez Jean-Yves Royer Bernard Pontoise Bertrand Sichler 《Tectonophysics》2008,454(1-4):70-85
To better understand the recent motion of the Pacific plate relative to the Rivera plate and to better define the limitations of the existing Rivera–Pacific plate motion models for accurately predicting this motion, total-field magnetic data, multibeam bathymetric data and sidescan sonar images were collected during the BART and FAMEX campaigns of the N/O L'Atalante conducted in April and May 2002 in the area surrounding the Moctezuma Spreading Segment of the East Pacific Rise, located offshore of Manzanillo, Mexico, at 106°16′W, between 17.8°N and 18.5°N. Among the main results are: (1) the principle transform displacement zone of the Rivera Transform is narrow and well defined east of 107o15′W and these azimuths should be used preferentially when deriving new plate motion models, and (2) spreading rates along the Moctezuma Spreading Segment should not be used in plate motion studies as either seafloor spreading has been accommodated at more than one location since the initiation of seafloor spreading in the area of the Moctezuma Spreading Segment, or this spreading center is not a Rivera–Pacific plate boundary as has been previously assumed. Comparison of observed transform azimuths with those predicted by the best-fit poles of six previous models of Rivera–Pacific relative motion indicate that, in the study area, a significant systematic bias is present in the predictions of Rivera–Pacific motion. Although the exact source of this bias remains unclear, this bias indicates the need to derive a new Rivera–Pacific relative plate motion model. 相似文献
306.
High-resolution clay-mineral analyses were performed on upper Hauterivian to lower Aptian sediments along a platform-to-basin transect through the northern Tethyan margin from the Neuchâtel area (Switzerland), to the Vocontian Trough (France) in order to investigate links between climate change, carbonate platform evolution, and fractionation patterns in clay minerals during their transport.During the Hauterivian, the northern Tethyan carbonate platform developed in a heterozoan mode, and the associated ramp-like topography facilitated the export of detrital material into the adjacent basin, where clay-mineral assemblages are dominated by smectite and kaolinite is almost absent, thereby suggesting dry-seasonal conditions. During the Late Hauterivian Balearites balearis ammonite zone, a change to a more humid climate is documented by the appearance of kaolinite, which reaches up to 30% of the clay fraction in sediments in the Vocontian Trough. This prominent change just preceded the Faraoni Oceanic Anoxic Event and the onset of the demise of the Helvetic Carbonate Platform, which lasted to the late early Barremian.From the Late Barremian onwards, the renewed growth of the northern Tethyan carbonate platform in a photozoan mode and the associated development of a marginally confined platform topography fractionated the clay-mineral assemblages exported into hemipelagic settings: kaolinite particles were preferentially retained in proximal, platform settings, due to their size and their relatively high specific weight. In the inner platform environment preserved in the Swiss Jura, an average of 32% of kaolinite in the clay fraction is observed during the latest Barremian–earliest Aptian, whereas clay-mineral assemblages of coeval sediments from deeper depositional settings are dominated by smectite and show only minor amounts of kaolinite.This signifies that besides palaeoclimate conditions, the morphology and ecology of the carbonate platform had a significant effect on the distribution and composition of clay assemblages during the Late Hauterivian–Early Aptian along the northern Tethyan margin. 相似文献
307.
Multi-hazard risk mapping and assessment on an active volcano: the GRINP project at Mount Cameroon 总被引:5,自引:4,他引:1
Pierre Thierry Laurent Stieltjes Emmanuel Kouokam Pierre Nguéya Paul M. Salley 《Natural Hazards》2008,45(3):429-456
To help improve the safety of its population faced with natural disasters, the Cameroon Government, with the support of the
French Government, initiated a programme of geological risk analysis and mapping on Mount Cameroon. This active volcano is
subject to a variety of hazards: volcanic eruptions, slope instability and earthquakes. Approximately 450,000 people live
or work around this volcano, in an area which includes one of Cameroon’s main economic resources. An original methodology
was used for obtaining the information to reply to questions raised by the authorities. It involves several stages: identifying
the different geological hazard components, defining each phenomenon’s threat matrix by crossing intensity and frequency indices,
mapping the hazards, listing and mapping the exposed elements, analysing their respective values in economic, functional and
strategic terms, establishing typologies for the different element-at-risk groups and assessing their vulnerability to the
various physical pressures produced by the hazard phenomena, and establishing risk maps for each of the major element-at-risk
groups (population, infrastructures, vegetation, atmosphere). At the end of the study we were able (a) to identify the main
critical points within the area, and (b) provide quantified orders of magnitude concerning the dimensions of the risk by producing
a plausible eruption scenario. The results allowed us to put forward a number of recommendations to the Cameroon Government
concerning risk prevention and management. The adopted approach corresponds to a first level of response to the authorities.
Later developments should make it possible to refine the quality of the methodology. 相似文献
308.
Aurlie Leroux Vincent Bichet Anne-Vronique Walter-Simonnet Michel Magny Thierry Adatte milie Gauthier Herv Richard Agns Baltzer 《Comptes Rendus Geoscience》2008,340(12):883-892
A sediment sequence (SP05, 12.5 m long) was taken from the deep zone of Lake Saint-Point (850 m a.s.l.). Sedimentological analyses highlight two main contrasted periods of sedimentation: the Last Glacial Maximum (LGM)/Late Glacial characterized by high silicates and quartz contents the Holocene dominated by the carbonated fraction. At the beginning of the Holocene (11 400 years cal. BP), silicates fraction flux abruptly decreased. The shift between the Late Glacial and the Holocene periods may be explained by forest development in the catchment. From 10 200 to 6800 years cal. BP, silicates and detrital carbonate fractions remained stable before they progressively increased steady till 5000 years cal. BP. Both increases cannot be totally attributed to an anthropic impact since pollen data indicate continuous anthropic activities only dated back from 3000 years cal. BP. They thus resulted from a dominant climatic control. From 5000 years cal. BP, silicates content still increased while detrital carbonates input became steady due to a change in pedogenetic processes affecting the catchment. During the last millennium, silicates and detrital carbonate decreased, probably due to pastureland development. 相似文献
309.
310.
Impacts of post‐glacial rebound on landslide spatial distribution at a regional scale in northern Iceland (Skagafjörður) 下载免费PDF全文
Etienne Cossart Denis Mercier Armelle Decaulne Thierry Feuillet Helgi Páll Jónsson Þorsteinn Sæmundsson 《地球表面变化过程与地形》2014,39(3):336-350
In de‐glaciated areas, para‐glaciation (i.e. the conditioning of landscapes by prior glaciation) has often been considered a major predisposing factor in landslide occurrence; its consequences have been particularly well identified at a fine scale (especially on bedrock jointing). Hitherto, the relative impacts of para‐glaciation on hillslope dynamics at a regional scale had nevertheless not been quantified statistically. We examine Skagafjörður area (northern Iceland) where landslides are widespread (at least 108 were mapped in an area of c. 3000 km2). We compare the role of para‐glaciation (debuttressing, influence of post‐glacial rebound) with that of classic factors (topography, lithology, etc.) in landslide occurrence and location, using a spatial analysis based on a chi‐square test. On the one hand, the results highlight that landslides are over‐represented in areas where post‐glacial rebound was at its maximum, with a stronger concentration of landslides in the northern part of the fjord. On the other hand, the distribution of landslides did not show any clear relationship with the pattern of glacial debuttressing. Tschuprow coefficient highlights that the influence of post‐glacial rebound on landslide location is higher than the combined influence of slope gradient, curvature or geological structure. This result is supported by our initial evidence for the timing of landslides in the area: most landslides occurred during the first half of the Holocene, and a period of hillslope instability was initiated when the post‐glacial uplift was at its maximum. Finally, the mechanisms that link post‐glacial rebound and landsliding as well as the geomorphic impacts of landslides, are discussed. Copyright © 2013 John Wiley & Sons, Ltd. 相似文献