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81.
N. V. Isaev V. M. Kostin G. G. Belyaev O. Ya. Ovcharenko E. P. Trushkina 《Geomagnetism and Aeronomy》2010,50(2):243-255
The measurements on board the Cosmos-1809 satellite of various parameters of the topside ionosphere plasma during more than
ten typhoons in various regions are analyzed. It is shown that specific zones of increased pressure of the electron gas, electric
field, and intense ion oscillations are formed during the intensification stage. In some cases the “typhoon eye” is formed
over the tropical depression zone in the ionosphere, that is, the region with sharply decreased plasma density and pressure
is observed a day and more prior to the moment when it happens in the atmosphere. 相似文献
82.
V.A. Belyaev M.A. Gornova A.Ya. Medvedev N.N. Pakhomova 《Russian Geology and Geophysics》2012,53(4):321-333
The Baidarik block of the Dzavhan microcontinent (Central Asian Fold Belt) includes the Upper Archean Baidaragin gray-gneiss complex. Among gray plagiogneisses, there are metabasic bodies, which are probably relics of early volcanics. By composition, the metabasites are divided into three petrochemical groups, whose protoliths were tholeiitic basalts, Al-undepleted and Al-depleted basaltic komatiites. Only a few samples are similar in REE composition to these protoliths. We have found metabasites with crustal-contamination features. The unusual geochemical properties of the metabasites (LREE enrichment and Nb, Zr, and Ti depletion) are related to their metasomatism. 相似文献
83.
84.
A. Yu. Lein P. N. Makkaveev A. S. Savvichev M. D. Kravchishina N. A. Belyaev O. M. Dara M. S. Ponyaev E. E. Zakharova A. G. Rozanov M. V. Ivanov M. V. Flint 《Oceanology》2013,53(5):570-606
The biogeochemical processes participating in the transformation of the particulate matter into sediment along the Yenisei River-St. Anna Trough (Kara Sea) meridional profile were studied using hydrochemical, geochemical, microbiological, radioisotope, and isotope methods. The water-sediment contact zone consists of three subzones: the suprabottom water, the fluffy layer, and the surface sediment. The total number, biomass, and integral activity of the microorganisms (dark 14CO2 assimilation) in the fluffy layer are usually higher than in the suprabottom water and sediment. The fluffy layer shows a decrease in the oxygen content and the growth of the dissolved biogenic elements. It was provided by the particulate organic matter supporting the vital activity of the heterotrophs from the overlying water column and by the flux of reduced compounds (NH4, H2S, CH4, Fe2+, Mn2+, and others) from the underlying sediments. The Corg isotopic composition of the fluffy layer and the sediments is 2–4 ‰ heavier than that of the particulate matter and sediment due to the presence of the isotopically heavy biomass of microorganisms. A change in the isotopic composition of the Corg in the fluffy layer and surface sediment as compared to the Corg of the particulate matter is a widespread phenomenon in the Arctic shelf seas and proves the leading role of microorganisms in the transformation of the particulate matter into sediment. 相似文献