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941.
Abstract: This article explores environmental imaginaries of colonization in lowland Canterbury. In 1844 Edward Shortland observed that his Māori companions had an exceptionally detailed geographical knowledge of the area and its resources, yet a few years later European settlers were viewing it as an empty stage on which to envision newly‐constructed landscapes. The terrain was contested, but colonial ‘improvement’, through the creation of spaces of modernity, took no cognizance of this. The legacies of that transformation are a simplified, orderly landscape, and fractured but persistent memories of indigenous ecosystems that are now being revived. 相似文献
942.
Steven L. Reneau Paul G. Drakos Danny Katzman Daniel V. Malmon Eric V. McDonald Randall T. Ryti 《地球表面变化过程与地形》2004,29(10):1209-1223
Sediment‐borne contamination in a watershed can be highly variable as a result of ?uvial processes operating over a range of time scales. This study presents a detailed analysis of the distribution of one contaminant along an ephemeral stream after 55 years of sediment transport, deposition, and exchange by ?ash ?oods. Wastewater containing plutonium was discharged into the Pueblo Canyon watershed from 1945 until 1964, and plutonium concentrations in ?uvial deposits vary over ?ve orders of magnitude. These variations can be attributed to three primary factors: time since contaminant releases, particle‐size sorting, and mixing of sediment from different sources. The highest concentrations occur in ?ne‐grained sediment deposits near the source that date to the period of ef?uent releases, and concentrations are lower in younger deposits, in coarser‐grained deposits, and in deposits farther downstream. The spatial distribution of plutonium is strongly affected by longitudinal variations in the size of sediment deposits of different age. A major aggradation–degradation cycle in the lower canyon overlapped with the period of active ef?uent releases, and a signi?cant portion of the total plutonium inventory is contained within large coarse‐grained deposits below ?ll terraces that post‐date 1945. The spatial pattern of contamination is thus determined by the speci?c geomorphic history of the watershed, in addition to processes of mixing and sorting during transport that occur in all ?uvial systems. Copyright © 2004 John Wiley & Sons, Ltd. 相似文献
943.
Nicholas J. Tate Chris Brunsdon Martin Charlton A. Stewart Fotheringham Claire H. Jarvis 《Journal of Geographical Systems》2005,7(3-4):273-290
This paper reports on the smoothing/filtering analysis of a digital surface model (DSM) derived from LiDAR altimetry for part of the River Coquet, Northumberland, UK using loess regression and the 2D discrete wavelet transform (DWT) implemented in the S-PLUS and R statistical packages. The chosen method of analysis employs a simple method to generate ‘noise’ which is then added to a smooth sample of LiDAR data; loess regression and wavelet methods are then used to smooth/filter this data and compare with the original ‘smooth’ sample in terms of RMSE. Various combinations of functions and parameters were chosen for both methods. Although wavelet analysis was effective in filtering the noise from the data, loess regression employing a quadratic parametric function produced the lowest RMSE and was the most effective. 相似文献
944.
A finite element model (namely TELEMAC) with a range of mesh refinements and assumptions of coastal water depths is used to
determine an optimal mesh for computing the M
2 tide in a region of significant geographical extent. The region adopted is the west coast of Britain covering the Irish and
Celtic Seas. The nature of the spatially varying topography and tidal distribution, together with a comprehensive set of measurements
and existing accurate finite difference model makes it ideal for such a study. Calculations show that a water-depth dependent
criterion for determining element size gives an optimal distribution over the majority of the region. However, local refinements
in narrow channels such as the North Channel and Bristol Channel are required. Although the specification of a zero coastal
water depth, leads to a fine near coastal grid, this does not yield the most accurate solution. In addition the computational
cost is high. In practice in a large area model the use of a non-zero coastal water depth yields optimum accuracy at minimal
computational cost. However, calculations show that accuracy is critically dependent upon nearshore water depths. Comparison
with the finite difference model shows that the bias in elevation amplitude in the finite difference solution is removed in
the finite element calculation. 相似文献
945.
Complete mantle section of a slow-spreading ridge-derived ophiolite: An example from the Isabela ophiolite in the Philippines 总被引:2,自引:0,他引:2
Abstract The Isabela ophiolite shows a complete ophiolite sequence exposed along the eastern coast of northern Luzon, the Philippines. It forms the Cretaceous basement complex for the northeastern Luzon block. This ophiolite is located at the northern end of a trail of ophiolites and ophiolitic bodies along the eastern margin of the Philippine Mobile Belt. This paper presents new findings regarding the nature and characteristics of the Isabela ophiolite. Peridotites from the Isabela ophiolite are relatively fresh and are composed of spinel lherzolites, clinopyroxene-rich harzburgites, depleted harzburgites and dunites. The modal composition, especially the pyroxene content, defines a northward depletion trend from fertile lherzolite to clinopyroxene-rich harzburgites and more refractory harzburgites. Variation in modal composition is accompanied by petrographic textural variations. The chromium number of spinel, an indicator of the degree of partial melting, concurs with petrographic observations. Furthermore, the Isabela ophiolite peridotites are similar in spinel and olivine major-element geochemistry and clinopyroxene rare earth-element composition to abyssal peridotites from modern mid-oceanic ridges. Petrological and mineral compositions suggest that the Isabela ophiolite is a transitional ophiolite subtype, with the fertile lherzolites representing lower sections of the mantle column that are usually absent in most ophiolitic massifs. The occurrence of the fertile peridotite presents a rare opportunity to document the lower sections of the ophiolitic mantle. The variability in composition of the peridotites in one continuous mantle section may also represent a good analogy of the melting column in the present-day mid-oceanic ridges. 相似文献
946.
Late Devonian (385−370 Ma) granitoid intrusions in the Meguma Zone of southwestern Nova Scotia represent two geographically separate magmatic suites that show subtly different lithological, geochemical and isotopic characteristics. “Central intrusions” crop out with satellite mafic-intermediate intrusions, range in composition from granodiorite to leucogranite, contain two micas, have exclusively peraluminous compositions (molar A/CNK 1.1-1.3), variably high values for FeOT (0.4–6.0 wt.%), Ba (5–980 ppm), Y (6–50 ppm), Pb (2–50 ppm), Ga (11–53 ppm), 87Sr/86Sri (0.7081-0.7130), δ18O (9.8–13.0) and δ34S (4.5–11.9), in conjunction with low values for εNd (−1 to −6.5). In contrast, “peripheral plutons” crop out with synplutonic mafic-intermediate intrusions, range in composition from tonalite to leucogranite, may contain minor hornblende, have dominantly peraluminous compositions (molar A/CNK 0.9-1.3), variably high concentrations of TiO2 (0.1-1.1 wt.%), Al2O3 (12.0–19.7 wt.%), CaO (0.2–4.9 wt.%), Sr (7–720 ppm), Cr (3–111 ppm) and V (1–136 ppm), higher εNd values (−2.0 to 3.2), and lower values for 87Sr/86Sri (0.7040-0.7079), δ188O (7.6–10.5) and δ34S (0–4.6). Such regional diversity is explained by inferring that upper crustal contamination dominated the central granitoid compositions and mixing with mantle-derived mafic-intermediate magmas dominated peripheral granitoid compositions. However, additional contributions from heterogeneous lower crust cannot be excluded. 相似文献
947.
Progressive hybridisation between Late Devonian mafic-intermediate and felsic magmas in the Meguma Zone of Nova Scotia, Canada 总被引:2,自引:0,他引:2
Marcus C. Tate D. Barrie Clarke Larry M. Heaman 《Contributions to Mineralogy and Petrology》1997,126(4):401-415
Two felsic plutons of Late Devonian (385–370 Ma) age in the Meguma Zone of southwestern Nova Scotia contain three circa 376
Ma synplutonic mafic-intermediate intrusions that collectively record progressive stages of in situ hybridisation. A 5 m wide
spessartite dyke in the Port Mouton Pluton probably underwent rapid cooling and crystallisation immediately after intrusion,
which heated and coarsened the adjacent tonalite. An 85 m long sheet of pillowed kersantite (also in tonalite of the Port
Mouton Pluton) presumably contained residual magma after quenching and obtained K, P, Ba, Rb, more radiogenic Sr, Zr, Nb,
and light REE from the tonalite during magma mingling. The third synplutonic body, a >100 m wide diorite sheet, intrudes granodiorite
of the adjacent Shelburne Pluton and has a circa 45 m wide gradational contact of metaluminous hornblende-tonalite. This tonalite
dominantly records magma mixing by the transfer of Ti, Mg, Fe, Ca, and V in hornblende, biotite, plagioclase, and (at least
in part) apatite xenocrysts derived from dioritic pillows that were originally disaggregated in the granodiorite, probably
in response to convection. Scattered data points, unusual “concave-down” variation trends for Al2O3, P2O5, and Sr, and non-hyperbolic Sr-Nd isotopic characteristics in the tonalite, apparently reflect syn- or post-mixing fractionation
and accumulation of xenocrysts from residual magma. Phosphorus may have assisted diffusion of Sr, Zr, Nb, and light REE, and
caused premature quenching of the hybrids at Mcleods Cove and Birchtown, during magma mingling and mixing.
Received: 1 January 1996 / Accepted: 3 August 1996 相似文献
948.
Blas L. Valero-Garcés Kathleen R. Laird Sherilyn C. Fritz Kerry Kelts Emi Ito Eric C. Grimm 《Quaternary Research》1997,48(3):359-369
Seismic stratigraphy, sedimentary facies, pollen stratigraphy, diatom-inferred salinity, stable isotope (δ18O and δ13C), and chemical composition (Sr/Ca and Mg/Ca) of authigenic carbonates from Moon Lake cores provide a congruent Holocene record of effective moisture for the eastern Northern Great Plains. Between 11,700 and 950014C yr B.P., the climate was cool and moist. A gradual decrease in effective moisture occurred between 9500 and 710014C yr B.P. A change at about 710014C yr B.P. inaugurated the most arid period during the Holocene. Between 7100 and 400014C yr B.P., three arid phases occurred at 6600–620014C yr B.P., 5400–520014C yr B.P., and 4800–460014C yr B.P. Effective moisture generally increased after 400014C yr B.P., but periods of low effective moisture occurred between 2900–280014C yr B.P. and 1200–80014C yr B.P. The data also suggest high climatic variability during the last few centuries. Despite the overall congruence, the biological (diatom), sedimentological, isotopic, and chemical proxies were occassionally out of phase. At these times the evaporative process was not the only control of lake-water chemical and isotopic composition. 相似文献
949.
950.
The subjectivity of ellipse fitting in many strain techniques has hindered the determination of fabric anisotropy and tectonic strain. However, many sets of x, y co-ordinates can be approximated as an ellipse using a least-squares algorithm to calculate a best-fit ellipse and associated average radial error. For instance, the two dimensional shape of many objects can be approximated as an ellipse by entering digitized co-ordinates of the object margin into the ellipse algorithm.The rim of maximum point density in a normalized Fry diagram is defined by normalized center-to-center distances between touching or nearly touching objects. The enhanced normalized Fry (ENFry) method automates ellipse fitting by entering center-to-center distances between these “touching” objects into the least-squares ellipse algorithm. For homogeneously deformed populations of 200 objects, the ENFry method gives an accurate and precise measure of whole-rock fabric anisotropy, particularly for low ellipticities. When matrix strain exceeds clast strain, manual ellipse fitting of normalized Fry plots gives more accurate matrix anisotropies.The mean object ellipse (MOE) method calculates the best-fit ellipse from the geometry of the objects. Three points from the margin of each object ellipse, centered at the origin and expanded or reduced to unit volume, are used to calculate the best-fit fabric ellipse. The MOE method is very precise for small data sets, making it a good method for mapping heterogenous object strain. However, least-squares calculations maximize the influence of distal and spurious ellipticities, causing the MOE method to overestimate the fabric ellipticity of most aggregates. 相似文献