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931.
Martín Jesús Rodríguez-Peces José Luis Pérez-García Julián García-Mayordomo José Miguel Aza?ón Juan Miguel Insua-Arévalo Jorge Delgado-García 《Natural Hazards》2011,59(2):1109-1124
In this paper, the applicability of the Newmark method at regional, sub-regional and site scales has been investigated in
the Lorca Basin (Murcia). This basin is located in one of the most seismically active regions of Spain. The area is very interesting
for studying earthquake-induced slope instabilities as there are well-known cases associated with specific earthquakes. For
the regional and sub-regional scales, a geographic information system has been used to develop an implementation of Newmark
sliding rigid block method. Soil and topographic amplification effects have been particularly considered. Subsequently, ‘Newmark
displacement’ maps for deterministic seismic scenarios have been produced. Some specific studies have also been performed
using limit equilibrium methods to estimate the safety factor and the critical acceleration of certain slope instabilities
at a site scale. These instabilities were the rock slides related to recent seismic series at the Lorca Basin: 2002 Bullas
(M
w = 5.0) and 2005 La Paca (M
w = 4.8). Finally, the safety factor, critical acceleration and Newmark displacement values estimated at different scales have
been compared to determine which scale is most suitable for the Newmark method. 相似文献
932.
933.
José C. García‐Gómez Carlos M. López‐Fé Free Espinosa José M. Guerra‐García Georgina A. Rivera‐Ingraham 《Marine Ecology》2011,32(1):6-14
The installation of urban and commercial infrastructures on the coast has a severe impact on the marine environment. This impact is mostly negative but, simultaneously, some of the species that colonize artificial substrata (sometimes rare or threatened) find refuge in man‐made structures. The protection of endangered species is usually provided by marine protected areas or by laws that punish their damage or collection, but effective enclosure and custody must be achieved in the case of easily accessible intertidal species. We used the ferruginous limpet, Patella ferruginea, as a case study because it is the most endangered invertebrate in the Mediterranean. This species, which lives in the intertidal zone and is very accessible to people, is a free‐spawning, protandric hermaphrodite, highly dependent on population density and individual size for its reproductive success. Previous work by the authors found the species is especially abundant on artificial substrates on both shores of the Strait of Gibraltar, where people collect fewer of them. Spanish laws of coastal management do not allow the enclosure of the natural coastline, but artificial installations like harbour breakwaters may be closed or guarded, and visits for educational purposes may be carried out under control. The possibility of declaring some kind of environmental protection for these artificial areas would be a very helpful tool for conservation and management purposes. Protected individuals would grow larger and eventually produce exponentially more offspring, which could be transported by currents to adjacent habitats. Here we propose a protection concept for artificial sites termed Artificial Marine Micro‐Reserve (AMMR), where some endangered species experience a refuge from human disturbance. This concept is a modification of the land micro‐reserves that have been recently declared in small natural sites that keep rare plant species. A network of AMMRs would be the final objective, allowing the creation of a great metapopulation of P. ferruginea and also giving refuge to other endangered species that have been found to grow in this type of substratum. Critically, the declaration of a micro‐reserve cannot be used as a reason in favour of new construction because of the negative influence of such structures on the marine environment, together with the fact that there is no certainty that valuable species will settle on them. 相似文献
934.
Takeshi Kozai Lydia Perelis-Grossowicz Annachiara Bartolini Chotima Yamee José Sandoval Francis Hirsch Keisuke Ishida Thasinee Charoentitirat Assanee Meesook Jean Guex 《Gondwana Research》2011,19(1):37-46
The paleontological investigations of the Jurassic of Western Thailand, districts of Mae Sot (Tak–Mae Sot highway, Padaeng Tak and Ban Mae Kut Luang Zinc mines) and Umphang (Klo Tho), provide age constraints for the Late Indosinian orogeny, the Paleotethys closure and the timing of the marine Jurassic inundation of Sundaland. The basal conglomerate of the Jurassic is derived from the pelagic Triassic Mae Sariang substratum. Stratigraphy, microfacies and paleontology of the Jurassic marine strata focus especially on ammonites, bivalves, large benthic foraminifera and algae. Among ammonites, the Tethyan Catulloceras perisphinctoides Gemmellaro marks the Upper Toarcian (Aalensis Zone) along the Tak–Mae Sot highway and Riccardiceras longalvum (Vacek), Malladaites pertinax (Vacek), Abbasites sp. and Vacekia sp. indicate Middle Aalenian to lowermost Bajocian in the Padaeng Mine (SE of Mae Sot) and Klo–Tho (Umphang). Vacekia sp., Spinammatoceras schindewolfi Linares and Sandoval and Malladaites vaceki Linares and Sandoval indicate Middle Aalenian to lowermost Upper Aalenian at Ban Mae Kut Luang (NE of Mae Sot). Among foraminifers, the large benthic foraminifer Timidonella sarda Bassoullet, Chabrier and Fourcade in the Western Tethys is indicative for Aalenian–Bajocian times, as characterized in the section at the Tak–Padaeng Zinc mine and the Klo–Tho Formation near Umphang. The endemic foraminifer Gutnicella kaempferi characterizes the Pu Khloe Khi Formation near Umphang. Among bivalves, shallow marine, dominantly endemic fauna includes Parvamussium donaiense (Mansuy) and Bositra ornate (Quenstedt), from the Toarcian to the Early Bajocian. A consideration of the faunal affinity shows that the fauna is partly endemic with Northern Tethyan (Eurasian) affinity. 相似文献
935.
Laura González-Acebrón R. H. Goldstein Ramón Mas José Arribas 《International Journal of Earth Sciences》2011,100(8):1811-1826
Stratigraphic relations, detailed petrography, microthermometry of fluid inclusions, and fine-scale isotopic analysis of diagenetic
phases indicate a complex thermal history in Tithonian fluvial sandstones and lacustrine limestones of the Tera Group (North
Spain). Two different thermal events have been recognized and characterized, which are likely associated with hydrothermal
events that affected the Cameros Basin during the mid-Cretaceous and the Eocene. Multiple stages of quartz cementation were
identified using scanning electron microscope cathodoluminescence on sandstones and fracture fills. Primary fluid inclusions
reveal homogenization temperatures (Th) from 195 to 350°C in the quartz cements of extensional fracture fillings. The high
variability of Th data in each particular fluid inclusion assemblage is related to natural reequilibration of the fluid inclusions,
probably due to Cretaceous hydrothermal metamorphism. Some secondary fluid inclusion assemblages show very consistent data
(Th = 281–305°C) and are considered not to have reequilibrated. They are likely related to an Eocene hydrothermal event or
to a retrograde stage of the Cretaceous hydrothermalism. This approach shows how multiple thermal events can be discriminated.
A very steep thermal gradient of 97–214°C/km can be deduced from δ18O values of ferroan calcites (δ18O −14.2/−11.8‰ V-PDB) that postdate quartz cements in fracture fillings. Furthermore, illite crystallinity data (anchizone–epizone
boundary) are out of equilibrium with high fluid inclusion Th. These observations are consistent with heat-flux related to
short-lived events of hydrothermal alteration focused by permeability contrasts, rather than to regional heat-flux associated
with dynamo-thermal metamorphism. These results illustrate how thermal data from fracture systems can yield thermal histories
markedly different from host-rock values, a finding indicative of hydrothermal fluid flow. 相似文献
936.
Paula M. Carreira Jos�� M. Marques Jorge Espinha Marques Helder I. Chamin�� Paulo E. Fonseca Fernando Monteiro Santos Rui M. Moura Jos�� M. Carvalho 《Hydrogeology Journal》2011,19(1):117-131
In a multidisciplinary approach, geological, geomorphologic, structural, hydrogeochemical and isotopic surveys were conducted on the Serra da Estrela groundwater system (central Portugal) in order to establish/develop a conceptual circulation model of the Caldas de Manteigas thermomineral system. A detailed study of the isotopic and geochemical composition of surface waters (e.g. Zêzere River), shallow groundwaters (cold dilute springs), and thermomineral waters was carried out to characterize the distribution of isotopes in waters of this mountainous region, and to determine the origin and possible recharge locations of the thermomineral system. Special attention was dedicated to isotopic tracers and their role in the definition of the thermomineral waters??conceptual model, considering: (1) the δ18O fractionation gradient; (2) the mean isotopic composition of the thermomineral waters in the region; and (3) the estimation of snowmelt contribution as a source of groundwater recharge at Serra da Estrela. The recharge of the thermomineral aquifer takes place on the more permeable zones of the granitic massif, associated with the main tectonic structures, whereas the recharge of the shallow aquifers seems to take place mostly in the plateaus, although another part of the recharge may occur in the slopes of the Zêzere River valley. 相似文献
937.
Induced polarization,resistivity, and self-potential: a case history of contamination evaluation due to landfill leakage 总被引:2,自引:1,他引:1
José Domingos Faraco Gallas Fabio Taioli Walter Malagutti Filho 《Environmental Earth Sciences》2011,63(2):251-261
This article compares the efficiency of induced polarization (IP) and resistivity in characterizing a contamination plume
due to landfill leakage in a typical tropical environment. The resistivity survey revealed denser electrical current flow
that induced lower resistivity values due to the high ionic content. The increased ionic concentration diminished the distance
of the ionic charges close to the membrane, causing a decrease in the IP phenomena. In addition, the self-potential (SP) method
was used to characterize the preferential flow direction of the area. The SP method proved to be effective at determining
the flow direction; it is also fast and economical. In this study, the resistivity results were better correlated with the
presence of contamination (lower resistivity) than the IP (lower chargeability) data. 相似文献
938.
939.
RésuménLes Gneiss de Torrox font partie de l’Unité de Sayalonga, appartenant au Complexe Alpujarride des Cordillères Bétiques (Espagne). Ils ont subi une déformation hétérogène par cisaillement simple, caractérisée par le développement de zones mylonitiques à pendage subhorizontal et de linéations d’étirement de direction N070°E. Nous interprétons ces linéations comme la direction de transport dans un contexte de chevauchements ductiles vers l’Kst-Nord-est. Ce sens de mouvement est très répandu dans les Alpujarrides, et permet de mieux comprendre que les nappes Alpujarrides occidentales soient plus métamorphiques que celles des Alpujarrides centrales et orientales. 相似文献
940.
AbstractThe Campo de Dalias is an emerged portion of the Alboran Sea, located on its northeastern margin. The study of this basin and its surrounding offshore areas reveals the structure on the region, whose outstanding feature is the N70-80E anticline extending from Guardias Viejas to Roquetas and continuing eastward under the sea. The other parts of the structure are characterized by several fault sets, the most important of which are those of N 70-9OE, N 120E and N45E direction. Some of these fault sets of originally different ages later replayed throughout the late Miocene up to the Quaternary. These replays seem to have occurred in approximately N-S compressive situations.The main compressive events took place in the latest Torto-nian and early Pleistocene. Between these two events a stage of considerable subsidence in the Pliocene basin can be detected, which caused the accumulation of sediments over a thousand metres thick in some places. Equally, we can detect an important uplift of the surrounding reliefs coeval with subsidence. Two transgressive situations are recorded and two important eustatic falls and partial emersion of the basin margin, mainly during the Messinian. 相似文献