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101.
Alcides Nobrega Sial Claudio Gaucher Marinho Alves da Silva Filho Valderez P. Ferreira Marcio M. Pimentel Luiz D. Lacerda Emmanoel V. Silva Filho Wilker Cezario 《Precambrian Research》2010
Two cap carbonates overlying glaciogenic diamictites crop out extensively in the eastern Vaza Barris Domain of the Sergipano Belt, northeastern Brazil. They are represented by carbonates of the Jacoca Formation, resting on top of diamictite of the Ribeiropolis Formation, and by the Olhos D’Agua Formation (carbonates, organic-rich towards the top), which overlies diamictite of the Palestina Formation. These two sequences were deformed and metamorphosed at sub-greenschist facies-conditions during the Brasiliano cycle (650–600 Ma). 相似文献
102.
We consider a restricted three-body problem where the primaries are moving in an elliptic collision orbit and the infinitesimal
mass moves in a three dimensional space. This paper is devoted to prove analytically the existence of several families of
symmetric periodic solutions as continuation of Keplerian circular orbits. In our approach the perturbing parameter is related
with the energy of the primaries. 相似文献
103.
Denudation history of the Bocaina Plateau, Serra do Mar, southeastern Brazil: Relationships to Gondwana breakup and passive margin development 总被引:1,自引:0,他引:1
Silvio T. Hiruma Claudio Riccomini May C. Modenesi-Gauttieri Peter C. Hackspacher Julio C. Hadler Neto Ana O.B. Franco-Magalhes 《Gondwana Research》2010,18(4):674-687
The Bocaina Plateau, which is situated on the eastern flank of the continental rift of southeastern Brazil, is the highest part of the Serra do Mar. Topographic relief in this area is suggested to be closely related to its complex tectono-magmatic evolution since the breakup of Western Gondwana and opening of the South Atlantic Ocean. Apatite fission track ages and track length distributions from 27 basement outcrops were determined to assess these hypotheses and reconstruct the denudation history of the Bocaina Plateau. The ages range between 303 ± 32 and 46 ± 5 Ma, and are significantly younger than the stratigraphic ages. Mean track lengths vary from 13.44 ± 1.51 to 11.1 ± 1.48 μm, with standard deviations between 1.16 and 1.83 μm. Contrasting ages within a single plateau and similar ages at different altitudes indicate a complex regional tectonothermal evolution. The thermal histories inferred from these data imply three periods of accelerated cooling related to the Early Cretaceous continental breakup, Early Cretaceous alkaline magmatism, and the Paleogene evolution of the continental rift of southeastern Brazil. The oldest fission track ages (> 200 Ma) were obtained in the Serra do Mar region, suggesting that these areas were a long-lived source of sediments for the Paraná, Bauru, and Santos basins. 相似文献
104.
Paulo Cesar Fernandes-da-Silva Ricardo Vedovello Claudio Jose Ferreira John Canning Cripps Maria Jose Brollo Amelia Joao Fernandes 《Environmental Earth Sciences》2010,61(8):1657-1675
Geo-environmental terrain assessments and territorial zoning are useful tools for the formulation and implementation of environmental
management instruments (including policy-making, planning, and enforcement of statutory regulations). They usually involve
a set of procedures and techniques for delimitation, characterisation and classification of terrain units. However, terrain
assessments and zoning exercises are often costly and time-consuming, particularly when encompassing large areas, which in
many cases prevent local agencies in developing countries from properly benefiting from such assessments. In the present paper,
a low-cost technique based on the analysis of texture of satellite imagery was used for delimitation of terrain units. The
delimited units were further analysed in two test areas situated in Southeast Brazil to provide estimates of land instability
and the vulnerability of groundwater to pollution hazards. The implementation incorporated procedures for inferring the influences
and potential implications of tectonic fractures and other discontinuities on ground behaviour and local groundwater flow.
Terrain attributes such as degree of fracturing, bedrock lithology and weathered materials were explored as indicators of
ground properties. The paper also discusses constraints on- and limitations of- the approaches taken. 相似文献
105.
Soil-precipitation feedbacks during the South American Monsoon as simulated by a regional climate model 总被引:1,自引:0,他引:1
Anna A. Sörensson Claudio G. Menéndez Patrick Samuelsson Ulrika Willén Ulf Hansson 《Climatic change》2010,98(3-4):429-447
We summarize the recent progress in regional climate modeling in South America with the Rossby Centre regional atmospheric climate model (RCA3-E), with emphasis on soil moisture processes. A series of climatological integrations using a continental scale domain nested in reanalysis data were carried out for the initial and mature stages of the South American Monsoon System (SAMS) of 1993–92 and were analyzed on seasonal and monthly timescales. The role of including a spatially varying soil depth, which extends to 8 m in tropical forest, was evaluated against the standard constant soil depth of the model of about 2 m, through two five member ensemble simulations. The influence of the soil depth was relatively weak, with both beneficial and detrimental effects on the simulation of the seasonal mean rainfall. Secondly, two ensembles that differ in their initial state of soil moisture were prepared to study the influence of anomalously dry and wet soil moisture initial conditions on the intraseasonal development of the SAMS. In these simulations the austral winter soil moisture initial condition has a strong influence on wet season rainfall over feed back upon the monsoon, not only over the Amazon region but in subtropical South America as well. Finally, we calculated the soil moisture–precipitation coupling strength through comparing a ten member ensemble forced by the same space–time series of soil moisture fields with an ensemble with interactive soil moisture. Coupling strength is defined as the degree to which the prescribed boundary conditions affect some atmospheric quantity in a climate model, in this context a quantification of the fraction of atmospheric variability that can be ascribed to soil moisture anomalies. La Plata Basin appears as a region where the precipitation is partly controlled by soil moisture, especially in November and January. The continental convective monsoon regions and subtropical South America appears as a region with relatively high coupling strength during the mature phase of monsoon development. 相似文献
106.
Resolution effects on regional climate model simulations of seasonal precipitation over Europe 总被引:5,自引:2,他引:3
We analyze a set of nine regional climate model simulations for the period 1961–2000 performed at 25 and 50 km horizontal
grid spacing over a European domain in order to determine the effects of horizontal resolution on the simulation of precipitation.
All of the models represent the seasonal mean spatial patterns and amount of precipitation fairly well. Most models exhibit
a tendency to over-predict precipitation, resulting in a domain-average total bias for the ensemble mean of about 20% in winter
(DJF) and less than 10% in summer (JJA) at both resolutions, although this bias could be artificially enhanced by the lack
of a gauge correction in the observations. A majority of the models show increased precipitation at 25 km relative to 50 km
over the oceans and inland seas in DJF, JJA, and ANN (annual average), although the response is strongest during JJA. The
ratio of convective precipitation to total precipitation decreases over land for most models at 25 km. In addition, there
is an increase in interannual variability in many of the models at 25 km grid spacing. Comparison with gridded observations
indicates that a majority of models show improved skill in simulating both the spatial pattern and temporal evolution of precipitation
at 25 km compared to 50 km during the summer months, but not in winter or on an annual mean basis. Model skill at higher resolution
in simulating the spatial and temporal character of seasonal precipitation is found especially for Great Britain. This geographic
dependence of the increased skill suggests that observed data of sufficient density are necessary to capture fine-scale climate
signals. As climate models increase their horizontal resolution, it is thus a key priority to produce high quality fine scale
observations for model evaluation. 相似文献
107.
Kurt Lambeck Anthony Purcell Nicholas. C. Flemming Claudio Vita-Finzi Abdullah M. Alsharekh Geoffrey N. Bailey 《Quaternary Science Reviews》2011,30(25-26):3542-3574
The history of sea level within the Red Sea basin impinges on several areas of research. For archaeology and prehistory, past sea levels of the southern sector define possible pathways of human dispersal out of Africa. For tectonics, the interglacial sea levels provide estimates of rates for vertical tectonics. For global sea level studies, the Red Sea sediments contain a significant record of changing water chemistry with implications on the mass exchange between oceans and ice sheets during glacial cycles. And, because of its geometry and location, the Red Sea provides a test laboratory for models of glacio-hydro-isostasy. The Red Sea margins contain incomplete records of sea level for the Late Holocene, for the Last Glacial Maximum, for the Last Interglacial and for earlier interglacials. These are usually interpreted in terms of tectonics and ocean volume changes but it is shown here that the glacio-hydro-isostatic process is an additional important component with characteristic spatial variability. Through an iterative analysis of the Holocene and interglacial evidence a separation of the tectonic, isostatic and eustatic contributions is possible and we present a predictive model for palaeo-shorelines and water depths for a time interval encompassing the period proposed for migrations of modern humans out of Africa. Principal conclusions include the following. (i) Late Holocene sea level signals evolve along the length of the Red Sea, with characteristic mid-Holocene highstands not developing in the central part. (ii) Last Interglacial sea level signals are also location dependent and, in the absence of tectonics, are not predicted to occur more than 1–2 m above present sea level. (iii) For both periods, Red Sea levels at ‘expected far-field’ elevations are not necessarily indicative of tectonic stability and the evidence points to a long-wavelength tectonic uplift component along both the African and Arabian northern and central sides of the Red Sea. (iv) The observational evidence is consistent with tectonic and isostatic processes both operating over the past 300,000 years without requiring changes in the time averaged (over a few thousand years) tectonic rates. (v) Recent bathymetric data for the Bab al Mandab region have been compiled to confirm the location and depth of the sill controlling flow in and out of the Red Sea. Throughout the last 400,000 years the Red Sea has remained open to the Gulf of Aden with cross sectional areas at times of glacial maxima about 2% of that today. (vi) The minimum channel widths connecting the Red Sea to the Gulf of Aden at times of lowstand occur south of the Hanish Sill. The channels are less than 4 km wide and remain narrow for as long as local sea levels are below ?50 m. This occurs for a number of sustained periods during the last two glacial cycles and earlier. (vii) Periods suitable for crossing between Africa and Arabia without requiring seaworthy boats or seafaring skills occurred periodically throughout the Pleistocene, particularly at times of favourable environmental climatic conditions that occurred during times of sea level lowstand. 相似文献
108.
Claudio 《Geoforum》2001,32(4)
This paper describes key urban development strategies pursued during the last seven years by the Municipality of Rio de Janeiro, the second largest city in Brazil. It discloses internal processes, organisational restructuring of the municipality and institutional changes geared to increase effective urban management and resource mobilisation required to implement multiple sector programmes and key projects in several locations in the city like Favela Bairro and Rio Cidade Programmes, The Rio Strategic Plan, etc. It is argued that the formation of interdepartmental working groups for better horizontal articulation of policy making and implementation, the creation of the financial and accounting unit, the decentralisation of authority towards sub-municipality levels, and capacity strengthening of its personnel – among other things – have made a positive impact on the performance of local government. The paper further highlights a significant change towards policies of urban consolidation and revitalisation of declined areas of the city supported by heavy public investments and the effort towards broader civil society involvement in municipal projects. Municipal autonomy, problem-solving and result-oriented type of planning and management and organisational change are some of the lessons pinpointed by the paper for a city of that size and complexity. 相似文献
109.
110.
Giovanni Bertolini Nicola Casagli Leonardo Ermini Claudio Malaguti 《Natural Hazards》2004,31(3):645-662
The Emilia Romagna slope of the Northern Apennines is strewnwith over 32,000 landslides, 5,000 of which are larger than 1 million cubic metres. They representthe remains of geomorphic agents that shaped the Apennines during the Holocene. Dating themby means of radiocarbon methods adds a contribution to the knowledge about the last periodof the geological geomorphological history of the Apennines. They can also be used to examinethe influence of Quaternary climatic changes on the instability of slopes and, for practicalor planning functions, to assess the periodicity of activity phases of the landslides. Thedating has been carried out on wood remnants buried under the landslide bodies. In some cases theentire tree trunk was found.In this paper we present radiocarbon dating of 20 casestudies in the Northern Apennines. Results range approximately from 13790–13670 cal y BP to950–790 cal`y BP. The oldest case is that of the Morsiano earth-flow, while the younger datedevent is represented by the Marano case that represents an example of how radiometric analysescan further enhance the available historical data. In the Cavola case, wood remnants of different ageswere found at different depths (from 9 to 45 m), allowing the dating of the first and followingperiods of activity of the landslide. The results are discussed and some considerations on the correlationbetween landslide occurrence and Holocene climate changes are proposed. 相似文献