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211.
The Albian to Santonian Colorado Group in the heavy oil area of Cold Lake, east-central Alberta represents a relatively condensed
section of shale-dominated sedimentation within the Western Interior Sea. These shales form the cap rock to the underlying
Clearwater and Grand Rapids formations that are exploited for bitumen extraction. Two cores covering the entire Colorado Group
provide a unique opportunity for establishment of a stratigraphic reference in an area that has received attention only for
its heavy oil-bearing Mannville Group. Based on sedimentology, geochemistry, micropaleontology, nannofossils, and wireline
log data, the Colorado Group was subdivided into the Joli Fou, Viking, Westgate, Fish Scales, Belle Fourche, Second White
Specks, and Niobrara formations. The Niobrara Formation was subdivided further into the Verger Member, informal Cold Lake
member, and First White Specks Member. Because of this region’s small accommodation space and distance to sources of coarse
clastic sediment, disconformities are indicated lithologically by bioclastic layers and missing biozones. Foraminiferal subzones
revealed two erosional boundaries associated with the Viking Formation. Faunal and floral evidence coupled with wireline log
correlations suggest that the Middle to Upper Turonian Carlile Formation, as described from southeastern Alberta, is missing.
That extends the Middle Turonian to Coniacian unconformity, as recognized in central Saskatchewan, westwards into Alberta. 相似文献
212.
213.
V. González-Quiñones A. de la Torre M. P. García A. Polo R. Jiménez-Ballesta 《Environmental Geology》2007,53(3):527-531
In the region of Castilla-La Mancha (Spain), over half of the soils are under cropping. This vast agricultural activity, combined
with other anthropological uses, has led to a deterioration of the soil quality and virtual degradation. Therefore, it was
deemed to assess the quality of these soils, which was achieved by applying two different methods. Three soils, representative
of typical conditions in this community, were sampled and diverse properties were analysed in order to apply two different
approaches. The first soil evaluation was carried out by a traditional method developed by FAO using a productivity index,
whereas the second method consisted of the application of a new method called SINDI, developed in New Zealand. Both approaches
make an evaluation based on a number of indicators that differs in each case. These differences explain why each method ranked
the soils studied in different order reaching diverse conclusions on their quality. 相似文献
214.
Arnoldo Valle-Levinson Nandita Sarkar Rosario Sanay Doris Soto Jorge León 《Estuaries and Coasts》2007,30(1):113-126
Underway current velocity profiles were combined with temperature and salinity profiles at fixed stations to describe tidal
and subtidal flow patterns in the middle of the northernmost Chilean fjord, Estuario Reloncaví. This is the first study involving
current velocity measurements in this fjord. Reloncaví fjord is 55 km long, 2 km wide, and on average is 170 m deep. Measurements
concentrated around a marked bend of the coastline, where an 8-km along-fjord transect was sampled during a semidiurnal tidal
cycle in March 2002 and a 2-km cross-fjord transect was occupied, also during a semidiurnal cycle, in May 2004. The fjord
hydrography showed a relatively thin (<5 m deep), continuously stratified, buoyant layer with stratification values >4 kg
m−3 per meter of depth. Below this thin layer, the water was relatively homogeneous. Semidiurnal tidal currents had low amplitudes
(<10 cm s−1) that allowed the persistence of a surface front throughout the tidal cycle. The front oscillated with a period of ca. 2.5
h and showed excursions of 2 km. The front oscillations could have been produced by a lateral seiche that corresponds to the
natural period of oscillation across the fjord. This front could have also caused large (2 h) phase lags in the semidiurnal
tidal currents, from one end of the transect to the other, within the buoyant layer. Tidal phases were relatively uniform
underneath this buoyant layer. Subtidal flows showed a 3-layer pattern consisting of a surface layer (8 m thick, of 5 cm s−1 surface outflow), an intermediate layer (70 m thick, of 3 cm s−1 net inflow), and a bottom layer (below 80 m depth, of 3 cm s−1 net outflow). The surface outflow and, to a certain extent, the inflow layer were related to the buoyant water interacting
with the ambient oceanic water. The inflowing layer and the bottom outflow were attributed to nonlinear effects associated
with a tidal wave that reflects at the fjord's head. The weak subtidal currents followed the morphology of the bend and caused
downwelling on the inside and upwelling on the outside part of the bend. 相似文献
215.
216.
Prem Chhetri Robert Stimson Jim Cooper Jonathan Corcoran Martin Bell David Pullar 《Transactions in GIS》2007,11(4):597-619
This article presents a GIS‐based methodology to integrate a measure of geographic attractiveness of localities in the process of allocating potential dwellings in the context of a large urban region. The methodology was developed for a study area in Brisbane‐South East Queensland (SEQ), known as the Sunbelt Region, a rapidly growing region and a popular tourist destination in Australia. In this article, we have used a multivariate technique to develop a set of parameterised linear equations to define underlying dimensions that drive residential location decision choices. Aesthetic and accessibility factors were identified in the factor analysis from data collected via a survey of Quality of Life. Spatial measures were based on a combination of network distance and kernel density estimation to calculate ‘aesthetic’ and ‘accessibility’ scenarios, which were then overlaid and multiplied by their subjective weights to create an ‘overall attractiveness scenario’. These development scenarios were integrated as a set of criteria to control the allocation of potential dwelling capacity over the next 25 years at a grid cell level. 相似文献
217.
Fossil remains of Euceratherium collinum (extinct shrub-ox) have been found throughout North America, including the Grand Canyon. Recent finds from the Escalante River Basin in southern Utah further extend the animal's range into the heart of the Colorado Plateau. E. collinum teeth and a metapodial condyle (foot bone) have been recovered in association with large distinctively shaped dung pellets, a morphology similar to a ‘Hershey's Kiss’ (HK), from a late Pleistocene dung layer in Bechan Cave. HK dung pellets have also been recovered from other alcoves in the Escalante River Basin including Willow and Fortymile canyons. Detailed analyses of the HK pellets confirmed them to be E. collinum and indicate a browser-type diet dominated (> 95%) by trees and shrubs: Artemisia tridentata (big sagebrush), Acacia sp. (acacia), Quercus (oak), and Chrysothamnus (rabbit brush). The retrieval of spring and fall pollen suggests E. collinum was a year-round resident in the Escalante River Basin. 相似文献
218.
Imprecise probabilities of climate change: aggregation of fuzzy scenarios and model uncertainties 总被引:1,自引:1,他引:1
Whilst the majority of the climate research community is now set upon the objective of generating probabilistic predictions
of climate change, disconcerting reservations persist. Attempts to construct probability distributions over socio-economic
scenarios are doggedly resisted. Variation between published probability distributions of climate sensitivity attests to incomplete
knowledge of the prior distributions of critical parameters and structural uncertainties in climate models. In this paper
we address these concerns by adopting an imprecise probability approach. We think of socio-economic scenarios as fuzzy linguistic
constructs. Any precise emissions trajectory (which is required for climate modelling) can be thought of as having a degree
of membership in a fuzzy scenario. Next, it is demonstrated how fuzzy scenarios can be propagated through a low-dimensional
climate model, MAGICC. Fuzzy scenario uncertainties and imprecise probabilistic representation of climate model uncertainties
are combined using random set theory to generate lower and upper cumulative probability distributions for Global Mean Temperature
anomaly. Finally we illustrate how non-additive measures provide a flexible framework for aggregation of scenarios, which
can represent some of the semantics of socio-economic scenarios that defy conventional probabilistic representation. 相似文献
219.
Desert Potholes: Ephemeral Aquatic Microsystems 总被引:1,自引:0,他引:1
Marjorie?A.?ChanEmail author Katrina?Moser Jim?M.?Davis Gordon?Southam Kebbi?Hughes Tim?Graham 《Aquatic Geochemistry》2005,11(3):279-302
An enigma of the Colorado Plateau high desert is the “pothole”, which ranges from shallow ephemeral puddles to deeply carved
pools. The existence of prokaryotic to eukaryotic organisms within these pools is largely controlled by the presence of collected
rainwater. Multivariate statistical analysis of physical and chemical limnologic data variables measured from potholes indicates
spatial and temporal variations, particularly in water depth, manganese, iron, nitrate and sulfate concentrations and salinity.
Variation in water depth and salinity are likely related to the amount of time since the last precipitation, whereas the other
variables may be related to redox potential. The spatial and temporal variations in water chemistry affect the distribution
of organisms, which must adapt to daily and seasonal extremes of fluctuating temperature (0–60 °C), pH changes of as much
as 5 units over 12 days, and desiccation. For example, many species become dormant when potholes dry, in order to endure intense
heat, UV radiation, desiccation and freezing, only to flourish again upon rehydration. But the pothole organisms also have
a profound impact on the potholes. Through photosynthesis and respiration, pothole organisms affect redox potential, and indirectly
alter the water chemistry. Laboratory examination of dried biofilm from the potholes revealed that within 2 weeks of hydration,
the surface of the desiccated, black biofilm became green from cyanobacterial growth, which supported significant growth in
heterotrophic bacterial populations. This complex biofilm is persumably responsible for dissolving the cement between the
sandstone grains, allowing the potholes to enlarge, and for sealing the potholes, enabling them to retain water longer than
the surrounding sandstone. Despite the remarkable ability of life in potholes to persist, desert potholes may be extremely
sensitive to anthropogenic effects. The unique limnology and ecology of Utah potholes holds great scientific value for understanding
water–rock–biological interactions with possible applications to life on other planetary bodies. 相似文献
220.
The appearance of the Hα fibrils suggests the presence of magnetic fields inclined at noticeably non-radial angles in the Sun's chromosphere. We present evidence to suggest that these angles continue into the photosphere. The presence even of small non-radial inclinations can significantly affect the appearance of regions observed by a longitudinal magnetograph. In particular, a simple bipolar loop can appear unbalanced when viewed near the limb. We suggest that the observed polar signal may be nothing more than a geometric effect arising when a balanced but systematically aligned array of bipolar pairs is viewed at an angle. 相似文献