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排序方式: 共有819条查询结果,搜索用时 156 毫秒
811.
Paula C.S. Carvalho Ana M.R. Neiva Maria M.V.G. Silva Eduardo A. Ferreira da Silva 《Chemie der Erde / Geochemistry》2014
Waters from abandoned Sb-Au mining areas have higher Sb (up to 2138 μg L−1), As (up to 1252 μg L−1) and lower Al, Zn, Li, Ni and Co concentrations than those of waters from the As-Au mining area of Banjas, which only contain up to 64 μg L−1 As. In general, Sb occurs mainly as SbO3− and As H2AsO4−. In general, waters from old Sb-Au mining areas are contaminated in Sb, As, Al, Fe, Cd, Mn, Ni and NO2−, whereas those from the abandoned As-Au mining area are contaminated in Al, Fe, Mn, Ni, Cd and rarely in NO2−. Waters from the latter area, immediately downstream of mine dumps are also contaminated in As. In stream sediments from Sb-Au and As-Au mining areas, Sb (up to 5488 mg kg−1) and As (up to 235 mg kg−1) show a similar behaviour and are mainly associated with the residual fraction. In most stream sediments, the As and Sb are not associated with the oxidizable fraction, while Fe is associated with organic matter, indicating that sulphides (mainly arsenopyrite and pyrite) and sulphosalts containing those metalloids and metal are weathered. Arsenic and Sb are mainly associated with clay minerals (chlorite and mica; vermiculite in stream sediments from old Sb-Au mining areas) and probably also with insoluble Sb phases of stream sediments. In the most contaminated stream sediments, metalloids are also associated with Fe phases (hematite and goethite, and also lepidocrocite in stream sediments from Banjas). Moreover, the most contaminated stream sediments correspond to the most contaminated waters, reflecting the limited capacity of stream sediments to retain metals and metalloids. 相似文献
812.
813.
David Völker Jacob Geersen Eduardo Contreras-Reyes Javier Sellanes Silvio Pantoja Wolfgang Rabbel Martin Thorwart Christian Reichert Martin Block Wilhelm Reimer Weinrebe 《International Journal of Earth Sciences》2014,103(7):1765-1787
The continental shelf and slope of southern Central Chile have been subject to a number of international as well as Chilean research campaigns over the last 30 years. This work summarizes the geologic setting of the southern Central Chilean Continental shelf (33°S–43°S) using recently published geophysical, seismological, sedimentological and bio-geochemical data. Additionally, unpublished data such as reflection seismic profiles, swath bathymetry and observations on biota that allow further insights into the evolution of this continental platform are integrated. The outcome is an overview of the current knowledge about the geology of the southern Central Chilean shelf and upper slope. We observe both patches of reduced as well as high recent sedimentation on the shelf and upper slope, due to local redistribution of fluvial input, mainly governed by bottom currents and submarine canyons and highly productive upwelling zones. Shelf basins show highly variable thickness of Oligocene-Quaternary sedimentary units that are dissected by the marine continuations of upper plate faults known from land. Seismic velocity studies indicate that a paleo-accretionary complex that is sandwiched between the present, relatively small active accretionary prism and the continental crust forms the bulk of the continental margin of southern Central Chile. 相似文献
814.
Jos I Saiz Nuria Anadn Javier Cristobo Oscar Garca-Alvarez Gerardo Garca-Castrillo Eduardo Lpez Cruz Palacn Jess S Troncoso Ana Ramos 《海洋学报(英文版)》2013,32(6):47-55
Insular marine biotas are often richer in faunal diversity than those from the open sea in the same geographical region. The existence of particular island effects were tested under polar conditions by comparing infaunal benthic assemblages on Peter I Island with those of similar latitudes in the open ocean at the Bellingshausen Sea and also from the coast of the Antarctic Peninsula. Sampling was carried out aboard the R/V Hespérides during the expedition named BENTART-2003 from 24 January to 3 March 2003. Benthic samples were collected at 18 stations ranging from 90 to 2 044 m depth, using an USNEL-type box corer (BC) dredge. Representatives of 32 higher taxa of invertebrates were found. Univariate and multivariate analyses revealed various patterns in the data. First, significant differences in polychaete abundance were detected between the stations located in the open sea and the remaining sites (island plus mainland sites). Bivalve abundances were also distinct between island and mainland sampling sites. Sediment columns taken from the island seafloor exhibited the highest rate of bioturbation by the infauna. These findings confirm the model that islands develop distinct assemblages characterized by the enhancement of the benthic communities even in cold waters. Several abiotic factors were measured simultaneously at the seafloor and along the water column to investigate faunal distribution patterns. Significant correlations were found between the benthic assemblages and a combination of two environmental variables: "island effect" (measured as a categorical variable) and the redox state of sediments. Richer and more complex benthic assemblages were found in Peter I Island’s sea bottom, whereas the more depauperate bottoms remained in the open sea. 相似文献
815.
Taciana K. Pinto Melanie C. V. Austen Richard M. Warwick Paul J. Somerfield André M. Esteves Francisco J. V. Castro Verônica G. Fonseca‐Genevois Paulo J. P. Santos 《Marine Ecology》2013,34(3):257-268
Mangroves are highly productive environments that play important ecological and socioeconomic roles; however, they have been impacted to different degrees in most countries worldwide. The knowledge of which organisms inhabit this environment and their ecological interactions is the first step towards its conservation. The natural variability of environmental factors in mangroves provides numerous niches available to different species. Meiofauna have patchy patterns of distribution that are related to the availability of resources. Hence, meiofauna are expected to present a high diversity of different taxa occupying the different microhabitats offered by mangroves. This work aims to test the hypothesis that the assemblage structure of Nematoda varies significantly among mangrove microhabitats and to contribute knowledge on the meiofauna diversity in mangrove environments. This work was carried out in a mangrove region at Pernambuco state, Northeastern Brazil. Qualitative samples were collected in nine microhabitats which show different characteristics mainly in terms of presence of vegetation or another organism and sediment grain size. Univariate and multivariate analysis were applied to Nematoda genera abundance data. Our results demonstrate the existence of significant differences among microhabitats regarding nematode assemblage structure corroborating the hypothesis. Different Nematoda assemblages are present in at least seven microhabitats. These assemblages are composed of nematode genera with different trophic and morphological features, demonstrating a strong relationship between morphological diversity and ecological plasticity. Furthermore, this study also demonstrates the importance of the conservation of this ecosystem and its attributes. 相似文献
816.
胶东苏鲁地体范家埠金矿成矿作用与矿床成因浅析:兼与胶北地体金矿对比 总被引:2,自引:0,他引:2
范家埠金矿是胶东半岛苏鲁地体内规模最大的石英脉型金矿。含金石英脉中锆石阴极发光和LA-ICP-MS微量元素及U-Pb同位素分析结果表明,含金石英脉中的锆石均为捕获围岩(新元古代威海片麻状花岗岩)的岩浆锆石,其中15个颗粒在U-Pb图解上位于谐和线上,其206Pb/238U加权平均年龄为(726±14)Ma(MSWD=4.6);另外7颗锆石位于不一致线上,其上交点年龄为(758±25)Ma,下交点年龄为(123±11)Ma(MSWD=0.45)。这些锆石的下交点年龄与金矿脉旁侧斜闪煌斑岩脉的角闪石40Ar/39Ar年龄分别为(118.8±1.6)Ma和(117.5±1.5)Ma,在误差范围内一致,表明范家埠金矿的成矿时代为120Ma左右。由此认为,苏鲁地体和胶北地体的金矿成矿作用均发生于早白垩世晚期120Ma前后,与目前多数人认为的华北克拉通岩石圈减薄的峰期时间一致,表明苏鲁地体的金矿成矿受岩石圈减薄的构造背景控制。范家埠金矿床成矿流体具中高温、中高盐度15.5%~23.2%(NaCleq)、低δ18OH2O(-3.84‰~-4.05‰)和低δDH2O(-82.5‰~-80.8‰)值等特点,载金矿物黄铁矿富32S(δ34S=-5.5‰~-9.1‰),与含油气盆地热卤水的组成相近,暗示范家埠金矿的成矿流体可能来源于中生代胶莱盆地。这种盆地流体沿断裂——五莲—米山深大断裂及其次级构造迁移,同时萃取基底岩石中的金形成含矿热液并在还原的环境中成矿。相反,胶北地体大量金矿床成矿流体具有低盐度、高δ18OH2O和δDH2O,δ34S(‰)为正值等特点。胶北和苏鲁地体早白垩世金成矿强度和成矿作用的差异可能反映了两者在地壳基底、流体来源和成矿环境等方面的不同。 相似文献
817.
Eleonora S. Carol Eduardo Emilio Kruse Jorge L. Pousa 《Environmental Earth Sciences》2010,60(4):749-756
Although not well known, the eco-hydrological functions of deep aquifers (those having no contact with surface hydrological
events) play an important role in the hydrological regime because they can affect the type of habitats, the availability of
water and nutrients and the salinity of the medium, among other environmental features. This work aims at characterizing the
deep Tertiary hydrogeological units of the Salado sedimentary basin in the Province of Buenos Aires, Argentina, at a regional
scale, and to determine their environmental importance in the hydrological cycle. The geological characterization of the study
area is based on the drilling profiles from oil exploration wells bored by different oil companies between 1948 and 1994,
and also from the existing literature. The conclusion is that water exchange between quaternary surface aquifers in contact
with atmospheric events and deep tertiary aquifers is one of the main processes that keep the hydrologic balance of the region.
Not only is this crucial for the conservation of the numerous and well-developed ecosystems in the basin wetlands, but also
significant for the agricultural and cattle-raising activities of the region. 相似文献
818.
Mariangela G. Praça Leite Maria Augusta Gonçalves Fujaco Hermínio A. NaliniJr. Paulo de Tarso A. Castro 《Environmental Earth Sciences》2010,60(8):1723-1730
In all geological scenarios, mineral water reactions will affect the water chemistry. As such, water resources in different
rocks commonly involve different hydrogeological compartments. The aim of this work is to evaluate the influence of geology
in the geochemistry signature of Itacolomi State Park waters. To do so, a survey of the geological units in the area was carried
out, a geological/stratigraphic division was made, and its correlation with the main geological events was determined. Using
the advantages of GIS, all the catchments were delimited. Based on this division, near 30 stream and lake segments were chosen
for analyses. In each point, all physiochemical properties of the water were measured, and samples were collected to determine
the concentrations of major and trace elements by ICP–OES. The dynamics of the Itacolomi State Park rock-soil and stream water
solutions suggest that mixing of drainage waters from different bedrock and soil sources regulates stream water physical–chemical
parameters and solute concentrations. The analytical data showed a clear correlation between the chemical compositions of
the solute and the geological characteristics of the catchment. Units that are covered by iron oxide hardpan (Manso unit)
and iron-banded formations (Custódio unit) show a large amount of soluble elements, including high values of Fe and Mn. On
the other hand, the presence of high values of Al and K (Itacolomi unit) are a direct consequence of the presence of quartzite
associated with low pH values. 相似文献
819.
Al-Qadami Ebrahim Hamid Hussein Mustaffa Zahiraniza Shah Syed Muzzamil Hussain Matínez-Gomariz Eduardo Yusof Khamaruzaman Wan 《Natural Hazards》2022,110(1):325-348
Natural Hazards - Vehicles can be easily swept away by floodwaters once the flow velocity and depth reach certain critical limits, with probabilities toward fatality reported to be nearly 50%.... 相似文献