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751.
Dehydration of dioctahedral aluminous phyllosilicates: thermodynamic modelling and implications for thermobarometric estimates 总被引:1,自引:1,他引:0
Benoît Dubacq Olivier Vidal Vincent De Andrade 《Contributions to Mineralogy and Petrology》2010,159(2):159-174
We propose a solid-solution model for dioctahedral aluminous phyllosilicates accounting for the main compositional variations,
including hydration, observed in natural smectites, interlayered illite/smectite, illites, and phengites from diagenetic to
high-grade metamorphic conditions. The suggested formalism involves dehydrated micas and hydrated pyrophyllite-like thermodynamic
end-members. With these end-members, the equilibrium conditions of quartz + water + K-bearing mica-like phyllosilicates of
fixed 2:1 composition are represented by a line in P–T space along which the interlayer water content varies. The relevant thermodynamic properties required for the calculation
of equilibrium conditions were derived using a set of 250 natural data of known maximal temperature and pressure conditions,
which covers a range between 25°C and few MPa to 800°C and 5 GPa. The temperatures calculated at fixed pressure with our model
are in fair agreement with those reported in the literature for the 250 natural data. At low temperature and pressure, the
amount of interlayer water in K-deficient phengite and illite is predicted to reach 100% of the apparent vacancies, which
is consistent with previous values reported in the literature. Although the amount of interlayer water is predicted to decrease
with pressure and temperature, it is calculated to be significant in K-deficient phengite from LT–HP pelites metamorphosed
at about 350°C, 10 kbar. The presence of molecular water in the interlayer site of such phengites has been confirmed by FTIR
mapping. Its implications for P–T estimates are discussed. 相似文献
752.
Christophe Lécuyer Vincent Balter François Fourel Romain Amiot Olga Otero Gérard Panczer Rossana Martini 《Geochimica et cosmochimica acta》2010,74(7):2072-584
The oxygen isotope fractionation between the structural carbonate of inorganically precipitated hydroxyapatite (HAP) and water was determined in the range 10-37 °C. Values of 1000 ln α() are linearly correlated with inverse temperature (K) according to the following equation: 1000 ln α() = 25.19 (±0.53)·T−1 − 56.47 (±1.81) (R2 = 0.998). This fractionation equation has a slightly steeper slope than those already established between calcite and water (
[O’Neil et al., 1969] and [Kim and O’Neil, 1997]) even though measured fractionations are of comparable amplitude in the temperature range of these experimental studies. It is consequently observed that the oxygen isotope fractionation between apatite carbonate and phosphate increases from about 7.5‰ up to 9.1‰ with decreasing temperature from 37 °C to 10 °C. A compilation of δ18O values of both phosphate and carbonate from modern mammal teeth and bones confirms that both variables are linearly correlated, despite a significant scattering up to 3.5‰, with a slope close to 1 and an intercept corresponding to a 1000 ln α() value of 8.1‰. This apparent fractionation factor is slightly higher or close to the fractionation factor expected to be in the range 7-8‰ at the body temperature of mammals. 相似文献
753.
In this work, lowest-order Raviart–Thomas and Brezzi–Douglas–Marini mixed methods are considered for groundwater flow simulations.
Typically, mixed methods lead to a saddle-point problem, which is expensive to solve. Two approaches are numerically compared
here to allow an explicit velocity elimination: (1) the well-known hybrid formulation leading to a symmetric positive definite
system where the only unknowns are the Lagrange multipliers and (2) a more recent approach, inspired from the multipoint flux
approximation method, reducing low-order mixed methods to cell-centered finite difference schemes. Selected groundwater flow
scenarios are used for the comparison between hybrid and multipoint approaches. The simulations are performed in the bidimensional
case with a general triangular discretization because of its practical interest for hydrogeologists. 相似文献
754.
Vincent Sastre Jean-Luc Loizeau Jens Greinert Lieven Naudts Philippe Arpagaus Flavio Anselmetti Walter Wildi 《Swiss Journal of Geoscience》2010,103(1):33-42
The current topographic maps of the Rhone Delta—and of Lake Geneva in general—are mainly based on hydrographic data that were
acquired during the time of F.-A. Forel at the end of the nineteenth century. In this paper we present results of a new bathymetric
survey, based on single- and multi-beam echosounder data. The new data, presented as a digital terrain model, show a well-structured
lake bottom morphology, reflecting depositional and erosional processes that shape the lake floor. As a major geomorphologic
element, the sub-aquatic Rhone Delta extends from the coastal platform to the depositional fans of the central plain of the
lake at 310 m depth. 9 canyons cut the platform edge of the delta. These are sinuous (“meandering”) channels formed by erosional
and depositional processes, as indicated by the steep erosional canyon walls and the depositional levees on the canyon shoulders.
Ripples or dune-like morphologies wrinkle the canyon bottoms and some slope areas. Subaquatic mass movements are apparently
missing on the delta and are of minor importance on the lateral lake slopes. Morphologies of the underlying bedrock and small
local river deltas are located along the lateral slopes of Lake Geneva. Based on historical maps, the recent history of the
Rhone River connection to the sub-aquatic delta and the canyons is reconstructed. The transition from three to two river branches
dates to 1830–1840, when the river branch to the Le Bouveret lake bay was cut. The transition from two to one river branch
corresponds to the achievement of the correction and dam construction work on the modern Rhone River channel between 1870
and 1880. 相似文献
755.
Lassaad Mejri Vincent Regard Sébastien Carretier Stéphane Brusset Mahmoud Dlala 《Comptes Rendus Geoscience》2010,342(11):864-872
The present-day seismicity in northeastern Tunisia reported from permanent networks is of low to moderate magnitude. However, earthquakes are mentioned in the literature, specially a destructive one in the antique city of Utique. Geologic, seismic, and neotectonic investigations in this area show that the Utique fold is closely related to the recent tectonic activity in this region. Data show that the Utique fold is built on an east-west fault, and we found evidence of activity of this fault in the past 20 kyr. A seismic section and balanced cross-section show that the slip rate is of the order of 0.38 mm.yr−1. Our data show definitively the Late Pleistocene–Holocene activity of the Utique Fault; and we can predict the earthquake recurrence interval which should be of ∼103–104 yr. This high seismic risk zone deserves to be taken into account during the establishment of important regional development programs and in the application of seismic building codes. 相似文献
756.
Lynchets are ridges formed by erosion and sediment accumulation downstream of agricultural plots and offer valuable insights into past agricultural activity. These microtopographies cover vast areas and serve as indicators of historical changes in land use. As a result, their ubiquity across Europe makes them particularly interesting. In this study, we propose a geoarchaeological approach to analyze six lynchets, four in the Vosges Mountains and two on the Lorraine Plateau (France). The lynchets can be considered soil archives with no stratigraphic organization or chronological sequence from bottom to top, making it difficult to determine the age of the lynchets and identify changes in land use over time. To this end, we propose the analysis of historical and geo-historical archives combined with the “pedosedimentary” archives of lynchets through charcoal identification and dating combined with near-infrared spectroscopy to determine the age, vegetation, and past land use changes associated with lynchet landscapes. By combining these multiple data sources, we are better able to show the chronological development of these ancient agricultural systems and uncover valuable information on landscape history. Charcoal dating suggests a higher frequency of fires from the Middle Ages. The dating aligns with the regional dynamics of anthropogenic fires, indicating a potential use of fire for cultural purposes. We also demonstrate the difficulty of extrapolating the dating of a lynchet to the entire lynchet system. Our results highlight the difficulties of interpreting the formation and dating of lynchets and the lynchet system on the sole basis of charcoal analysis. However, we highlight the value of applying pedoanthracology to lynchets to determine the dynamics of land use change in former fields. 相似文献
757.
Gert Finger Frank Eisenhauer Reinhard Genzel Christopher Mandla Ian Baker Domingo Alvarez Antonio Amorim Wolfgang Brandner Christophe Dupuy Casey Deen Derek Ives Leander Mehrgan Manfred Meyer Karin Perraut Guy Perrin Jörg Stegmeier Christian Straubmeier Harald J. Weller Vincent Isgar 《Astronomische Nachrichten》2023,344(8-9):e20230069
Near-infrared adaptive optics as well as fringe tracking for coherent beam combination in optical interferometry require the development of high-speed sensors. Because of the high speed, a large analog bandwidth is required. The short exposure times result in small signal levels which require noiseless detection. Both requirements cannot be met by state-of-the-art conventional CMOS technology of near-infrared arrays as has been attempted previously. A total of five near-infrared SAPHIRA 320 × 256 pixel HgCdTe e−APD arrays have been deployed in the wavefront sensors and in the fringe tracker of the VLTI instrument GRAVITY. The current limiting magnitude for coherent exposures with GRAVITY is mk = 19, which is made possible with ADP technology. New avalanche photo-diode array (APD) developments since GRAVITY include the extension of the spectral sensitivity to the wavelength range from 0.8 to 2.5 μm. After GRAVITY a larger format array with 512 × 512 pixels has been developed for both AO applications at the ELT and for long integration times. Since dark currents of <10−3 e−/s have been demonstrated with 1Kx1K e−APD arrays and 2Kx2K e−APD arrays have already been developed, the possibilities and adaptations of e−APD technology to provide noiseless large-format science-grade arrays for long integration times are also discussed. 相似文献