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排序方式: 共有113条查询结果,搜索用时 31 毫秒
51.
P. Breen L.A. Robinson S.I. Rogers A.M. Knights G. Piet T. Churilova P. Margonski N. Papadopoulou E. Akoglu A. Eriksson Z. Finenko V. Fleming-Lehtinen B. Galil F. Goodsir M. Goren O. Kryvenko J.M. Leppanen V. Markantonatou S. Moncheva T. Oguz L. Paltriguera K. Stefanova F. Timofte F. Thomsen 《Marine Policy》2012
52.
N.J.T. Edberg A.I. Eriksson U. Auster S. Barabash A. Bößwetter C.M. Carr S.W.H. Cowley E. Cupido M. Fränz K.-H. Glassmeier R. Goldstein M. Lester R. Lundin R. Modolo H. Nilsson I. Richter M. Samara J.G. Trotignon 《Planetary and Space Science》2009,57(8-9):1085-1096
We present the first two-spacecraft near-simultaneous observations of the Martian bow shock (BS), magnetic pileup boundary (MPB) and photo-electron boundary (PEB) obtained by the plasma instruments onboard Rosetta and Mars Express during the Rosetta Mars flyby on February 25, 2007. Our observations are compared with shape models for the BS and MPB derived from previous statistical studies. The MPB is found at its expected position but the BS for this event is found significantly closer to the planet than expected for the rather slow and moderately dense solar wind. Cross-calibration of the density measurements on the two spacecraft gives a density profile through the magnetosheath, indicating an increasing solar wind flux during the Rosetta passage which is consistent with the multiple BS crossings at the Rosetta exit. 相似文献
53.
Mass occurrence of benthic coccoid cyanobacteria and their role in the production of Neoarchean carbonates of South Africa 总被引:1,自引:0,他引:1
Jzef Kazmierczak Wladyslaw Altermann Barbara Kremer Stephan Kempe Patrick G. Eriksson 《Precambrian Research》2009,173(1-4):79
The sparse Archean fossil record is based almost entirely on carbonaceous remnants of microorganisms cellularly preserved due to their early post-mortem silicification. Hitherto as an exception, sedimentary carbonate rocks from the Neoarchean Nauga Formation of South Africa contain calcified microbial mats composed of microbiota closely resembling modern benthic colonial cyanobacteria (Chroococcales and Pleurocapsales). Their remains, visible under the scanning electron microscope (SEM) after etching of polished rock samples, comprise capsular envelopes, mucilage sheaths, and groups of cells mineralized by calcium carbonate with an admixture of Al–K–Mg–Fe silicates. The capsular organization of the mucilaginous sheaths surrounding individual cells and cell clusters forming colonies and the mode of mineralization are the characteristic common features of the Neoarchean microbiota described and their modern analogues. The new findings indicate massive production of calcium carbonates by benthic coccoid cyanobacteria in the Neoarchean, and offer a solution to the problem of the origin of Archean carbonate platforms, stromatolites and microbial reefs. 相似文献
54.
55.
Topographic data sets are often composed of terrain samples arranged in irregular meshes. Many gradient estimation methods require the data to be arranged in a regular mesh; irregular meshes present a difficulty for them. This paper presents a novel method of estimating surface gradients from irregularly spaced inputs. The method is derived using directional derivatives and is shown to be a generalization of traditional finite difference methods. Analytical tests were used to evaluate the method, which was shown to be accurate and robust. 相似文献
56.
Summary The sky view factor (SVF) is used in forest, road and urban climatology to characterise radiative properties. We now propose
a method suitable for forest canopies using the raster based and commercially available software IDRISI. It uses quadratic
pixels in rows and columns in a scanned equiangular fish-eye image. A threshold value is chosen to divide the image into sky
and non-sky areas. The resulting image is then multiplied with a sky view weight image, where the weights of the pixels depend
on the angular distance from zenith. The sum of pixel products gives the SVF. Quality analysis of the method is also performed.
The choice of threshold value gives some uncertainties due to leaves reflecting sunlight. This error will be reduced by observing
details (branches etc.) in the image and by choosing an overcast day for capturing the image. The precision range for SVF
calculations will be better than 0.1.
Received November 22, 1999 Revised July 17, 2000 相似文献
57.
A 1600-m succession of quartz arenites and associated shaley deposits comprising the Hospital Hill Subgroup at the base of the Witwatersrand Supergroup is considered to have been deposited largely under the influence of tidal processes. Facies analysis indicates that deposition occurred in the following environments: (1) marine shalf; (2) shallow subtidal to intertidal; (3) intertidal flat; and (4) tidal inlet. The presence of strong tidal currents implies that the Witwatersrand Basin was open to an ocean basin, at least during the early stages of its evolution. Palaeocurrent trends and isopach data suggest that this probably lay to the southwest, an area now occupied by the high grade Natal—Namaqua metamorphic belt. The contrast between the supermature quartz arenites of the Hospital Hill Subgroup and the overlying gold-bearing immature subgreywackes, feldspathic quartzites and conglomerates of fluvial origin is believed to be a function of tidal reworking of sediments. 相似文献
58.
Second- and third-order fault-bounded Precambrian basins frequently host deposits of the sedimentary massive sulphide group.
Three-dimensional geometric modelling of the thickness of preserved basin-fill successions of the Transvaal Supergroup, using
DATAMINE software, and residual gravity modelling of the contemporary basement floor, help delineate areas of exploration
potential in this unit. Two main depositional axes are tentatively identified for the basal volcano-sedimentary protobasinal
Transvaal successions. A sheet-like geometry was indicated for the succeeding Black Reef sandstones and Chuniespoort Group
chemical sedimentary rocks. The uppermost Pretoria Group thickness model delineates eastern and western second-order basins
separated by a central submerged palaeohigh. A similar isopach pattern is noted for the thick shales of the Silverton Formation
in this group, with, in addition, a well-defined third-order basin in the northwest of the western second-order basin. The
residual gravity model indicates two linear palaeovalleys adjacent to this western basin, one coincident with one of the axes
inferred for the protobasinal rocks. The fault-bounded second- and third-order basins and depositional axes postulated here
are consistent with known geological data and suggested sedimentation models. Cumulative distortions implicit in the DATAMINE
computer modelling technique are reduced when the method is applied on the basin-wide scale, enabling identification of regional
exploration target areas rather than immediate prospecting targets.
Received: 14 August 1996 / Accepted: 13 March 1997 相似文献
59.
P. G. Eriksson 《Mineralium Deposita》1997,32(4):419-422
Sediment-hosted uranium ores at Henkries in northwest South Africa occur in fine-grained sands, carbonaceous muds and diatomaceous
earth within late Pleistocene lake deposits. The lakes are linked by short fluvial channel reaches and these aqueous beds
are encompassed in predominant aeolian dune deposits. The late Pleistocene fluvial-lacustrine-aeolian succession is succeeded
by a Holocene dune cover. Textural characterisation of lacustrine, fluvial and aeolian sands was based on volume percentages
observed in sediment settling tubes. Vortex action during Holocene dune migration contaminated these aeolian cover sands with
small amounts of substrate material, whose presence could be detected in settling tube patterns of surface aeolian sediment
samples. It was thus possible to map buried lacustrine ore bodies, which were shown, by a successful drilling programme, to
be displaced downwind.
Received: 28 August 1996 / Accepted: 3 September 1996 相似文献
60.
Version management is a prerequisite for digital information flow between phases in the planning and building processes. Information evolves over time and many parties retrieve information from the various phases. The aim of this article is to evaluate versioning methods, focusing on geodata buildings in the 3D cadastre process. The main attention in the evaluation is on the comprehensive ISO standard Product Lifecycle Support (PLCS). PLCS is evaluated against two simpler versioning methods, the versioning in CityGML 3.0 and a modified Git versioning method implemented in CityJSON. CityGML 3.0 fulfils all but one requirement and PLCS meets all. The methods vary in complexity; the Git proposal is a simple solution, easy to implement and maintain, while PLCS includes all functionalities and is complex to implement. There is a trade‐off between number of functionalities and complexity, it is therefore important that the intended purpose determines the choice of versioning method. 相似文献