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31.
A total of 284 ringed seals (Phoca hispida) were sampled to determine their diet in the spring of 1981 and 1982. Few seals contained identifiable stomach contents. No significant age-or sex-related differences in choice of prey were found. It seems that in spring northwestern Spitsbergen ringed seals prey upon arctic cod (Boreogadus saida) , decapods and larger amphipods.? Diet, ringed seal, Svalbard . 相似文献
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The South Auckland Volcanic Field is a Pleistocene (1·590·51Ma) basaltic intraplate, monogenetic field situated south ofAuckland City, North Island, New Zealand. Two groups of basaltsare distinguished based on mineralogy and geochemical compositions,but no temporal or spatial patterns exist in the distributionof various lava types forming each group within the field: GroupA basalts are silica-undersaturated transitional to quartz-tholeiiticbasalts with relatively low total alkalis (3·04·6wt %), Nb (729 ppm), and (La/Yb)N (3·47·6);Group B basalts are strongly silica-undersaturated basanitesto nepheline-hawaiites with high total alkalis (3·37·9wt %), Nb (32102 ppm), and (La/Yb)N (1247). GroupA has slightly higher 87Sr/86Sr, similar Nd, and lower 206Pb/204Pbvalues compared with Group B. Contrasting geochemical trendsand incompatible element ratios (e.g. K/Nb, Zr/Nb, Ce/Pb) areconsistent with separate evolution of Groups A and B from dissimilarparental magmas derived from distinct sub-continental lithosphericmantle sources. Differentiation within each group was controlledby olivine and clinopyroxene fractionation. Group B magmas weregenerated by <8% melting of an ocean island basalt (OIB)-likegarnet peridotite source with high 238U/204Pb mantle (HIMU)and enriched mantle (EMII) characteristics possibly inheritedfrom recycled oceanic crust. Group A magmas were generated by<12% melting of a spinel peridotite source also with HIMUand EMII signatures. This source type may have resulted fromsubduction-related metasomatism of the sub-continental lithospheremodified by a HIMU plume. These events were associated withMesozoic or earlier subduction- and plume-related magmatismwhen New Zealand was at the eastern margin of the Gondwana supercontinent. KEY WORDS: continental intraplate basalts; geochemistry; HIMU, EMII; Sr, Nd, and Pb isotopes; South Auckland; sub-continental lithospheric sources 相似文献
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RIDLEY W. IAN; RHODES J. M.; REID ARCH M.; JAKES P.; SHIH C.; BASS M. N. 《Journal of Petrology》1974,15(1):140-159
Basalt was successfully cored at Site 54 in the Parace VelaBasin of the Philippine Sea, and at Site 57 on the CarolineRidge as part of Leg 6 of the Deep Sea Drilling Project. Site54 basalts are altered, but selected major and trace elements,particularly REE allow their characterization as high-aluminaolivine tholeiites, with flat REE patterns, no Eu anomalies,and low dispersed trace-element contents. Basalt from Site 57is distinctly different, with higher TiO2, P2O5, Fe/Mg ratio,and dispersed trace elements, low Ni, Mg, and a strongly fractionatedREE pattern. Derivation by fractionation of transitional basaltis suggested. Varying degrees of alteration of Site 54 basalts has causeddepletion in MgO and addition of Rb, Sr, Ba, Ka2O, and Na2O.Mineralogically these changes have resulted in alteration ofolivine and pyroxene, but plagioclase and iron-titanium oxidesremain unaffected. Microprobe data are presented for olivine, clinopyroxene, plagioclase,Fe-Ti oxides, and chrome-spinel in all three basalts. In 544,548 pyroxenes are zoned from salite to ferroaugite, andshow erratic decrease in A12O3 and TiO2 with increasing ironcontent. In 572, pyroxenes are more magnesian than thosein site 54 basalts, and show an increase in A12O3 and TiO2 withiron-enrichment. The anomalous behaviour of Al2O3 and TiO2 insome clinopyroxenes, and the close textural relationship ofpyroxene and magnesian olivine in 572 basalt, suggestthese minerals are xenocrystic, and were incorporated duringmagma ascent. Spinels of picotite composition in early-formed,and possibly xenocrystic, olivine, and plagioclase crystallizedprior to magma eruption, and may have begun crystallizationwithin the mantle. Site 54 basalts add further confirmation that inter-are basaltsclosely resemble ocean ridge tholeiites, although there is apaucity of data from inter-are environments. Site 57 basaltis chemically and mineralogically distinct from ocean ridgebasalts and may be related to similar volcanics erupted on theCaroline Islands. 相似文献
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Chemical variation in biotite from the KJokken gabbro-syeniteintrusion in the Proterozoic Gardar province in South Greenlandhas been investigated by electron probe and, for F and Li, ionmicroprobe. Most mica occurs in small amounts as fringes onilmenomagnetite or fayalite, rarely as an intercumulus or poikiliticphase. The micas range continuously from Phlog70Ann30 in a gabbro,to Phlog4Ann96 in the most evolved (slightly persilicic andperalkaline) syenite. In the syenites Fe-Mg partitioning betweenbiotite and olivine can be described by a single distributioncoefficient, Kd = XF XBiotMs/XBiotFe 3, suggesting that thesereactant phases mix ideally at the reaction T. Experimentaldata for Fe-Mg exchange via aqueous chloride solutions (Schulien,1980) imply low T (32Q?C). F was absent in the experiments andmay significantly affect the exchange equilibrium. Kd in thegabbros is 1, consistent with equilibrium via a fluid depletedin F because of crystallization of large amounts of amphibole. Al, Mn, and Ti vary regularly throughout the series and canbe used as markers of cryptic variation in the layered syenites.(Al + Si): 22 O is always in the range 7.77.85. A1/(A1+ Si) decreases from 0.31 in gabbros to 0.25 in the most Fe-richmicas. Li is always < 260 ppm w. In the syenite series, Fshows a near-linear inverse relationship with Fe/(Fe + Mg) whichpasses close to OF at Ann100 with l.4 wt% F(07 F to 44positive charges) at Ann44. Biotites in the gabbro unit (whichforms an outer sheath to the intrusion) have relatively lessF, probably because it was consumed by coexisting amphibole.I8O is similar for both gabbros and syenites, and it is unlikelythat an envelope fluid was involved in the reactions. G reachesa maximum of 0.3 wt. % in biotite except for that in one syenitesample with 07 wt. %. Calculation of relative F-OH fugacitiesfrom the reaction OH-phlogopite + F-annite = F-phlogopite +OH-annite, as calibrated by Munoz (1984), appears to suggestthat each horizon in the layered series was in equilibrium witha slightly different fluid. In view of the intimate interleavingof these lithologies, this is improbable. The equilibrium constantof the exchange reaction, obtained from the experimental data,seems not to be appropriate to the Klokken assemblage, or toother examples of regular F-Fe avoidance. Explanations may includeshort-range Fe-Mg ordering in the natural examples or the effectof additional components in the fluid. F contents are high incomparison with biotites from calc-alkaline complexes; highmagmatic F may account for the igneous layering common in theGardar. Temperatures calculated from reactions involving fayaliteand magnetite show that most biotites grew subsolidus. The F-poorannites grew > 300 ?C subsolidus even when texturally intercumulus.Stable isotope data are consistent with the separation and retentionof a deuteric fluid during the final stage of magmatic crystallization.Klokken was not generally subject to the pervasive, long-range(in both distance and time) dydrothermal interactions demonstratedin calcalkaline and theleiitic intrusions, although more extensivefluid flow is indicated for the more permeable laminated syenites.The biotites preserve chemical variation indicating local equilibriumwith other mafic phases, and halogens provide a useful markerof subsolidus fluid flow. 相似文献
38.
IAN LITTLEWOOD 《水文科学杂志》2013,58(5):795-811
Abstract A continuous simulation rainfall-streamflow modelling approach that identifies unit hydrographs for total streamflow has been applied to an 11-year record from a national hydrometric monitoring network catchment in the UK. The model is of the parametrically parsimonious conceptual model (PPCM) type that can make efficient use of rainfall, streamflow and air temperature data readily available from established national and regional monitoring networks. A multiple split-sample model calibration and simulation analysis is presented that reveals some guiding principles for calibrating and applying PPCMs generally. The inadequacy of a one-dimensional objective function for calibrating best PPCMs is demonstrated. A two-dimensional objective function approach is superior but is shown to be unreliable in some cases, confirming the need for additional critical inspection of other model performance statistics, model parameters and time series plots as an integral part of the model calibration process. A strong tendency evident from the multiple split-sample analysis is that, for the catchment studied, models that fit relatively well in calibration mode perform relatively poorly in simulation mode. 相似文献
39.
On the effect of mid-air collisions on aeolian saltation 总被引:9,自引:0,他引:9
The effect of mid-air collisions on aeolian saltation is investigated using concentration profiles and grain velocities predicted by a numerical saltation model. The probability of a mid-air collision is found to be greater at high wind speeds. It is also found that mid-air collisions tend to reduce the number of grain/bed impacts and thus reduce the number of ejecta near the bed; this, in turn, reduces the intensity of mid-air collisions. It is suggested that this feed-back mechanism significantly influences transport rates at high wind speeds. 相似文献
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