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91.
W.I. Ridley A.M. Reid J.L. Warner R.W. Brown 《Physics of the Earth and Planetary Interiors》1973,7(2):133-136
Apollo 15 breccia 15427 and soils 15101, 15261 and 15301 contain abundant spheres and fragments of a green glass that is remarkably constant in composition. The glass is rich in Fe and Mg, and low in Ti, unlike any known lunar basalt, and may be derived from material of pyroxenitic composition in the Apennine Front. 相似文献
92.
Evidence is presented of a periodic component in the inter-annual variability of precipitation and pressure data for India
during June, the month of the onset of the Indian southwest monsoon. Two frequencies that explain a statistically significant
percent of the variance in these data sets are the same as the two that explain most of the variance of the average monthly
lunar tidal potential for June. Not only are the frequencies the same but they are also in phase which strongly suggests that
lunar tides in the atmosphere do, in fact, produce an element of climatic variability. The amplitude of the atmospheric response
to this periodic forcing was not constant in time but was found to be related to the long term change in northern hemispheric
surface temperature. This susceptibility of the atmosphere to an external forcing results in a nonlinear relationship between
forcing and response. As a result, nonlinear regression had to be used in order to adequately define the magnitude of the
response at a given frequency. The ramifications of this nonlinear response are discussed. The nonlinear interaction of the
northern hemisphere temperature and the 18.6 year lunar nodal cycle results in a modulation of the frequency which appears
in a linear spectral analysis near 22 years. Thus, the 22-year cycle often found in meteorological data sets may instead be
the result of the modulated nodal cycle. 相似文献
93.
Between 1973 and 1986 a group at the University of Wisconsin worked on the use of the periodic portion of climatic time series
with the aim of exploring the potential for year-or-more in advance forecasting. This paper reports on the real time verification
of the last sets of forecasts made by the group.
From spectra of temperature and cube-rooted precipitation the dominant frequencies were chosen. These were usually related
to tidal frequencies. A Fourier series of these dominant terms was then fitted to the dependent data set and future values
calculated. These were analyzed for forecast skill, and the skillful Fourier series retained. Real time forecasts were then
made. Verification shows a low probability that the forecast skills were obtained by chance. It is suggested that the periodic
term might be a useful addition to more standard approaches to long range forecasting. 相似文献
94.
Arch M. Reid R. W. Brown J. B. Dawson G. G. Whitfield J. C. Siebert 《Contributions to Mineralogy and Petrology》1976,58(2):203-220
Analyses are reported for garnet and pyroxene from 17 eclogites that contain diamond. The garnets contain small but significant contents of Na, Ti and P and the pyroxenes contain traces of K. The diamond-bearing eclogites do not constitute a unique compositional group but show a range of mineral compositions consistent with a very high P-T environment. 相似文献
95.
Major element, Rb, Sr, Ba, Cr and V analyses as well as 13 new rare earth element (REE) analyses are presented for the greywacke basement surrounding the Taupo Volcanic Zone (TVZ). On this basis the basement rocks are divided into a Western Basement of approximately andesitic composition ( 62% SiO2) and an Eastern Basement of approximately granodiorite composition ( 75% SiO2). These analyses, 5 new REE analyses for the rhyolites, and published data for the volcanic rocks of TVZ are used to investigate the petrogenesis of rhyolitic rocks in the area.Least-squares mixing calculations for major elements show that 88% fractional crystallisation of high-alumina basalt produces a liquid of rhyolitic bulk composition, but Rayleigh fractionation models show that the trace element concentrations of the rhyolites are inconsistent with basalt fractionation. 57% fractionation of the assemblage plagioclase (35.6%), orthopyroxene (9.7%), clinopyroxene (7.8%), ilmenite (0.6%) and magnetite (3.4%) from a plagioclase-pyroxene andesite can produce liquids of rhyolitic bulk composition. REE concentrations produced by this model are consistent with those observed in the rhyolites but predicted Ba and Rb values are lower and V concentrations are higher than those in the rhyolites. Andesite fractionation also produces an unrealistic fractionation of the Cr/V ratio.A non-modal melting model involving 35% melting of a granulitic assemblage (plagioclase + quartz + clinopyroxene + orthopyroxene + biotite + magnetite + cordierite) with a bulk composition equivalent to the Western Basement can reproduce the REE pattern of the rhyolites as well as the concentrations of Rb and Ba. Sr values remain anomalously high, but the Cr/V ratio does not indicate fractionation. Absolute values of Cr and V are within the uncertainties of published crystal—liquid partition coefficients. The rhyolites have relatively flat REE patterns (La/Yb 7.5), as do the greywackes (La/Yb 8.2), so it is therefore unlikely that the rhyolites equilibrated with a garnet or amphibole-bearing assemblage. 相似文献
96.
Philip C. Reid 《Marine pollution bulletin》1980,11(2):47-51
The incidence of Paralytic Shellfish Poisoning along the eastern seaboard of America has increased and spread during the last decade. One of the core areas for Paralytic Shellfish Poison (PSP), a poison that is derived from toxic dinoflagellates, is centred on the Bay of Fundy. It is in the upper reaches of the Bay of Fundy that a proposal has been made to construct a tidal power generation plant; this project would have a considerable effect on the water circulation, tidal regime and sedimentation characteristics of the Bay of Fundy and Gulf of Maine. Alterations such as these to the hydrography of this area may lead to changes in the occurrence of toxic dinoflagellates and the associated patterns and intensity of PSP. 相似文献
97.
John D. Reid 《Boundary-Layer Meteorology》1979,16(1):3-22
Vertical dispersion in the neutral surface layer is investigated using a Markov Chain simulation procedure. The conceptual basis of the procedure is discussed and computation procedures outlined. Wind and turbulence parameterizations appropriate to the neutral surface layer are considered with emphasis on the Lagrangian time scale. Computations for a surface release are compared with field data. Good agreement is found for the variation of surface concentration and cloud height to distances 500 m downwind of the source. The functional form of the vertical concentration profile is examined and an exponential with exponent 1.6 is found to give the best fit with simulations.For elevated releases, it is demonstrated that an initial dip of the mass mean height from the simulation can be normalized for various release heights using a non-dimensionalized downwind coordinate incorporating advective wind speed and wind shear. The vertical distribution standard deviation (
z
), as employed in Gaussian models, shows a fair degree of independence with source height but close examination reveals an optimum source height for maximum z at a given downwind distance,x. This source height increases with downwind distance. Also the simulations indicate that vertical wind shear is more important than vertical variation of Lagrangian time scale close to the source, with a reverse effect farther downwind. 相似文献
98.
Two Karroo dolerite sills display chemical and mineralogical variation compatible with cumulus enrichment. The Blaauwkrans sill is an olivine tholeiite and contains a central zone slightly enriched in olivine, plagioclase and clinopyroxene. The thicker Hangnest sill is a quartz tholeiite and shows evidence of crystal settling and has a lower zone enriched in cumulus orthopyroxene and plagioclase.The two sills differ quite markedly in their trace element compositions, with the Hangnest magma enriched by a factor of two in LIL elements (Rb, Ba, Nb, Zr, Y) relative to the Blaauwkrans magma. The Hangnest magma contained extremely low Ni contents (3–5 ppm), whereas the Blaauwkrans magma contained higher but more normal Ni (100–110ppm). Such contrasting trace element compositions preclude any simple genetic relationship between the two Karroo magmas but they may be related either through a common parent or are derivatives from separate parental magmas.South African Contribution No. 24 to the International Geodynamics Project 相似文献
99.
100.
D.L. Reid 《Journal of African Earth Sciences》1997,24(4):621-633
Igneous rocks of the Richtersveld Subprovince in South Africa and Namibia form a Palaeo-Mesoproterozoic arc complex, dominated by extrusive andesites and their plutonic equivalents (diorites, tonalites), although the whole spectrum of rock types from ultramafic to felsic is present. SmNd isotope data indicate an extrusion age of 2000 Ma, thereby confirming previously published RbSr and UThPb ages. Initial Nd, Sr and Pb isotope ratios indicate a juvenile crust-producing episode at this time, with rapid recycling of young crust to generate rhyolitic and granitic components within the arc complex. The Richtersveld Subprovince represents the oldest crust in the western Namaqua Province, which was subsequently recycled during post 2.0 Ga tectonothermal events, especially the 1200–1000 Ma Kibaran episode. 相似文献