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排序方式: 共有149条查询结果,搜索用时 453 毫秒
121.
Rik Noorlandt Pauline P. Kruiver Marco P. E. de Kleine Marios Karaoulis Ger de Lange Antonio Di Matteo Julius von Ketelhodt Elmer Ruigrok Benjamin Edwards Adrian Rodriguez-Marek Julian J. Bommer Jan van Elk Dirk Doornhof 《Journal of Seismology》2018,22(3):605-623
The seismic hazard and risk analysis for the onshore Groningen gas field requires information about local soil properties, in particular shear-wave velocity (VS). A fieldwork campaign was conducted at 18 surface accelerograph stations of the monitoring network. The subsurface in the region consists of unconsolidated sediments and is heterogeneous in composition and properties. A range of different methods was applied to acquire in situ VS values to a target depth of at least 30 m. The techniques include seismic cone penetration tests (SCPT) with varying source offsets, multichannel analysis of surface waves (MASW) on Rayleigh waves with different processing approaches, microtremor array, cross-hole tomography and suspension P-S logging. The offset SCPT, cross-hole tomography and common midpoint cross-correlation (CMPcc) processing of MASW data all revealed lateral variations on length scales of several to tens of metres in this geological setting. SCPTs resulted in very detailed VS profiles with depth, but represent point measurements in a heterogeneous environment. The MASW results represent VS information on a larger spatial scale and smooth some of the heterogeneity encountered at the sites. The combination of MASW and SCPT proved to be a powerful and cost-effective approach in determining representative VS profiles at the accelerograph station sites. The measured VS profiles correspond well with the modelled profiles and they significantly enhance the ground motion model derivation. The similarity between the theoretical transfer function from the VS profile and the observed amplification from vertical array stations is also excellent. 相似文献
122.
David Julius Völker 《Geo-Marine Letters》2010,30(5):541-547
123.
Jorge M. Gaspar-Escribano Manuel Navarro Belén Benito Antonio García-Jerez Francisco Vidal 《Bulletin of Earthquake Engineering》2010,8(6):1547-1567
An approach that relates results from a regional seismic hazard assessment study with local-scale site-effect characterizations
in an area of low-to-moderate seismic activity such as Andalusia (southern Spain), is presented. Results of a previous probabilistic
seismic hazard analysis of Andalusia on rock conditions are disaggregated to infer hazard controlling earthquakes for different
target motions. A collection of controlling magnitude-distance pairs and the corresponding site-specific response spectra
at main capital cities of the region are obtained. These spectra are first-order approximations to expected seismic actions
required in local earthquake risk assessments. In addition, results of independent, local-scale studies developed in Almeria
City (SE Andalusia) are used to derive an updated seismic zonation of the city. These include predominant soil period estimates
and shear-wave velocity profiles at different locations. If a local seismic risk assessment study or an earthquake-resistant
structural design is to be developed, it may be recommended the use of different seismic actions on sites characterized by
distinct response to seismic shaking (as derived from the seismic zonation). The seismic action related to worst-case scenarios
may be modeled through a hazard-consistent response spectrum, obtained by hazard disaggregation at the spectral acceleration
with period matching the prevailing resonant period of the target site or structure. 相似文献
124.
Melekestseva I. Yu. Maslennikov V. V. Ayupova N. R. Belogub E. V. Maslennikova S. P. Bel’tenev V. E. Danyushevsky L. Large R. 《Geology of Ore Deposits》2020,62(3):254-259
Geology of Ore Deposits - The formation of present-day seafloor sulfide deposits is accompanied by their continuous oxidation and crystallization of insoluble Fe oxyhydroxides, which absorb metals... 相似文献
125.
Maxime Virolle Benjamin Brigaud Raphaël Bourillot Hugues Fnis Eric Portier Thibault Duteil Julius Nouet Patricia Patrier Daniel Beaufort 《Sedimentology》2019,66(3):859-894
Porosity and permeability may be preserved in deep sandstone reservoirs by clay coating (mainly chlorite) which limits quartz overgrowths. Chloritization around quartz grains results mainly from mineralogical transformations of pre‐existing clays. It is fundamental to study those clay precursors to better understand and predict the location and distribution of clay coatings in subsurface sandstones for petroleum or geothermal prospecting. This paper reports a high‐resolution analysis of the composition, distribution and fabric of clays along a modern estuary, the Gironde (south‐west France). The scale of the study ranges from thin sections, through sand bar bodies, up to the entire estuary. Results show that clays are detrital and deposited at the same time as sand grains despite strong hydrodynamic conditions. Clays bind to medium‐grained sands forming detrital clay grain coats. On average, 26% of detrital sand grains are coated along the entire length of the estuary. Coat thickness varies from 1 μm to more than 200 μm, and coat coverage exceeds 30% in some samples. The turbidity maximum zone position (surface water turbidity from 1 to 10 g l?1) in the estuary, which is controlled by seasonal variations in hydrodynamic processes, significantly impacts the location of the maximum clay content and the abundance of coated grains in sandy facies along the estuary. Flocculation in the water column results in the accumulation of suspended matter and contributes to the high turbidity in the estuary. Exopolymeric substances produced by diatoms are observed both in the field and by cryo‐scanning electron microscopy, suggesting that they may play a major role in binding detrital clay around sand grains. Finally, tidal bars and heterolithic point bars in the estuary funnel and estuarine channels are prime sedimentological targets for finding clay coatings and potentially good reservoir quality in deeply buried sandstones. 相似文献
126.
127.
128.
Summer phytoplankton pigments and community composition related to water mass properties in the Gulf of Gabes 总被引:1,自引:1,他引:0
M. Bel Hassen Z. Drira A. Hamza H. Ayadi F. Akrout H. Issaoui 《Estuarine, Coastal and Shelf Science》2008,77(4):645-656
Variations in phytoplankton pigments and community composition were examined in the Gulf of Gabes in relationship to water mass properties, characterised by the influence of the Modified Atlantic Water and by the thermal stratification. Data were collected on board the R/V Hannibal during July 2005.Distinct water masses were identified using cluster analysis of temperature–salinity (T–S) characteristics. Three major clusters appeared based on the combined effects of temperature and salinity. The first cluster was identified as the cool and less salty bottom Modified Atlantic Water (MAW). The warmer and saltier Mediterranean Mixed Water (MMW) represented the second cluster. The third cluster was the Transition Water (TW) separating the two previous clusters.The pigment and taxonomic composition of these water masses were examined. Chlorophyll a was rather low (<200 ng l−1). Chlorophyll b was generally the most abundant accessory pigment and fucoxanthin dominated the accessory pigments in the MAW. Proportions of chlorophyll a associated with different phytoplankton classes were estimated using CHEMTAX software, and did not present significant variations among water groups. The results pointed out variations in the relative contribution of each phytoplankton taxa in each station group. Chlorophytes and prasinophytes accounted for 65% of chlorophyll a in the MMW. Diatoms and chlorophytes were relatively abundant in the MAW contributing to almost 63% of chlorophyll a. An unstructured community, slightly dominated by prasinophytes, chlorophytes and cryptophytes, characterised the TW. Different trophic statuses were observed in these water masses, the MMW and the MAW being characterised by mesotrophy, while an oligotrophy was observed in the TW. Nutrient availability, particularly the P-limitation supported by the summer stratification, as revealed by the high N:P ratio (greater than 20), seems to enhance the development of small-sized phytoplankton, thereby supporting the regenerated production. 相似文献
129.
Feki-Sahnoun Wafa Njah Hasna Hamza Asma Barraj Nouha Mahfoudi Mabrouka Rebai Ahmed Bel Hassen Malika 《Ocean Dynamics》2020,70(7):897-911
Ocean Dynamics - The blooms of the toxic dinoflagellate Karenia selliformis can be predicted with accuracy derived from knowledge of the main forcing variables. A naive Bayes classifier modeling... 相似文献
130.
Florence Schubotz Julius S. Lipp Sabine Kasten Matthias Zabel Kai-Uwe Hinrichs 《Geochimica et cosmochimica acta》2011,75(16):4377-4415
At the Chapopote Knoll in the Southern Gulf of Mexico, deposits of asphalt provide the substrate for a prolific cold seep ecosystem extensively colonized by chemosynthetic communities. This study investigates microbial life and associated biological processes within the asphalts and surrounding oil-impregnated sediments by analysis of intact polar membrane lipids (IPLs), petroleum hydrocarbons and stable carbon isotopic compositions (δ13C) of hydrocarbon gases. Asphalt samples are lightly to heavily biodegraded suggesting that petroleum-derived hydrocarbons serve as substrates for the chemosynthetic communities. Accordingly, detection of bacterial diester and diether phospholipids in asphalt samples containing finely dispersed gas hydrate suggests the presence of hydrocarbon-degrading bacteria. Biological methanogenesis contributes a substantial fraction to the methane captured as hydrate in the shallow asphalt deposits evidenced by significant depletion in 13C relative to background thermogenic methane. In sediments, petroleum migrating from the subsurface stimulates both methanogenesis and methanotrophy at a sulfate-methane transition zone 6-7 m below the seafloor. In this zone, microbial IPLs are dominated by archaeal phosphohydroxyarchaeols and archaeal diglycosidic diethers and tetraethers. Bacterial IPLs dominate surface sediments that are impregnated by severely biodegraded oil. In the sulfate-reduction zone, diagnostic IPLs indicate that sulfate-reducing bacteria (SRB) play an important role in petroleum degradation. A diverse mixture of phosphohydroxyarchaeols and mixed phospho- and diglycosidic archaeal tetraethers in shallow oil-impregnated sediments point to the presence of anaerobic methane-oxidizing ANME-2 and ANME-1 archaea, respectively, or methanogens. Archaeal IPLs increase in relative abundance with increasing sediment depth and decreasing sulfate concentrations, accompanied by a shift of archaeol-based to tetraether-based archaeal IPLs. The latter shift is suggested to be indicative of a community shift from ANME-2 and/or methanogenic archaea in shallower sediments to ANME-1/methanogenic archaea and possibly benthic archaea in deeper sediments. 相似文献