全文获取类型
收费全文 | 13104篇 |
免费 | 534篇 |
国内免费 | 177篇 |
专业分类
测绘学 | 285篇 |
大气科学 | 1079篇 |
地球物理 | 3040篇 |
地质学 | 4725篇 |
海洋学 | 1129篇 |
天文学 | 2048篇 |
综合类 | 52篇 |
自然地理 | 1457篇 |
出版年
2022年 | 61篇 |
2021年 | 175篇 |
2020年 | 211篇 |
2019年 | 236篇 |
2018年 | 336篇 |
2017年 | 331篇 |
2016年 | 387篇 |
2015年 | 331篇 |
2014年 | 432篇 |
2013年 | 714篇 |
2012年 | 462篇 |
2011年 | 652篇 |
2010年 | 571篇 |
2009年 | 716篇 |
2008年 | 597篇 |
2007年 | 583篇 |
2006年 | 509篇 |
2005年 | 454篇 |
2004年 | 453篇 |
2003年 | 451篇 |
2002年 | 385篇 |
2001年 | 279篇 |
2000年 | 307篇 |
1999年 | 228篇 |
1998年 | 235篇 |
1997年 | 195篇 |
1996年 | 205篇 |
1995年 | 188篇 |
1994年 | 175篇 |
1993年 | 161篇 |
1992年 | 142篇 |
1991年 | 102篇 |
1990年 | 136篇 |
1989年 | 118篇 |
1988年 | 130篇 |
1987年 | 142篇 |
1986年 | 129篇 |
1985年 | 165篇 |
1984年 | 192篇 |
1983年 | 171篇 |
1982年 | 161篇 |
1981年 | 121篇 |
1980年 | 104篇 |
1979年 | 116篇 |
1978年 | 110篇 |
1977年 | 97篇 |
1976年 | 92篇 |
1975年 | 100篇 |
1974年 | 88篇 |
1973年 | 98篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
911.
912.
Tadashi Kito Sebastian Rost Christine Thomas Edward J. Garnero 《Geophysical Journal International》2007,169(2):631-645
Broad-band P - and S -waves from earthquakes in South America recorded at Californian network stations are analysed to image lateral variations of the D"-discontinuity beneath the Cocos plate. We apply two array processing methods to the data set: a simplified migration method to the P -wave data set and a double-array method to both the P - and S -wave data sets, allowing us to compare results from the two methods. The double-array method images a dipping reflector at a depth range from 2650 to 2700 km in the southern part of the study area. We observe a step-like topography of 100 km to a shallower reflector at about 2600 km depth to the north, as well as evidence for a second (deeper) reflector at a depth range from 2700 to 2750 km in the north. Results from the simplified migration agree well with those from the double-array method, similarly locating a large step in reflector depth in a similar location (about 2650 km depth in the south and about 2550 km in the north) as well as the additional deeper reflector at the depth of about 2750 km in the north. Waveform modelling of the reflected waves from both methods suggests a positive velocity contrast for S waves, but a negative velocity contrast for P waves for the upper reflector in agreement with predictions from mineral physical calculations for a post-perovskite phase transition. The data also show some evidence for the existence of another deeper reflector that could indicate a double intersection of the geotherm with the post-perovskite stability field, that is, the back-transformation of post-perovskite to perovskite close to the core–mantle boundary. 相似文献
913.
914.
915.
Thirty-seven new K–Ar ages from West Maui volcano, Hawai‘i, are used to define the waning stages of shield growth and a brief
episode of postshield volcanism. All but two samples from shield-stage strata have reversed polarity magnetization, so conceivably
the exposed shield is not much older than the Olduvai Normal-Polarity subchron, or about 1.8 Ma. The oldest ages obtained
are in the range 1.9–2.1 Ma but have large analytical error. Shield volcanism ended about 1.35 Ma, and postshield volcanism
followed soon thereafter, persisting until about 1.2 Ma. Exposed shield-stage strata were emplaced at a rate of about 0.001 km3 per year, a rate smaller than historic Hawaiian magmatic rates by a factor of 100. Stratigraphic accumulation rates are similar
to those measured previously at Wai‘anae volcano (O‘ahu) or the upper part of the Mauna Kea shield sequence (Hilo drill core,
Hawai‘i). These rates diminish sharply during the final 0.3–0.5 m.y. of the shield stage. Hawaiian shield volcanoes begin
waning well before their last 0.5 m.y. of life, then end quickly, geologically speaking, if West Maui is representative. 相似文献
916.
Gert Lube Shane J. Cronin Thomas Platz Armin Freundt Jonathan N. Procter Cargill Henderson Michael F. Sheridan 《Journal of Volcanology and Geothermal Research》2007
Small-volume pyroclastic density currents (PDCs) are generated frequently during explosive eruptions with little warning. Assessing their hazard requires a physical understanding of their transport and sedimentation processes which is best achieved by the testing of experimental and numerical models of geophysical mass flows against natural flows and/or deposits. To this end we report on one of the most detailed sedimentological studies ever carried out on a series of pristine small-volume PDC deposits from the 1975 eruption of Ngauruhoe volcano, whose emplacement were also witnessed during eruption. Using high-resolution GPS surveys, a series of lateral excavations across the deposits, and bulk sedimentological analysis we constrained the geomorphology, internal structure and texture of the deposits with respect to laterally varying modes of deposition. 相似文献
917.
An eruption on the eastern flank of Piton de la Fournaise volcano started on 16 November, 2002 after 10 months of quiescence.
After a relatively constant level of activity during the first 13 days of the eruption, lava discharge, volcanic tremor and
seismicity increased from 29 November to 3 December. Lava effusion suddenly ceased on 3 December while shallow earthquakes
beneath the Dolomieu summit crater were still recorded at a rate of about one per minute. This unusual activity continued
and increased in intensity over the next three weeks, ending with the formation of a pit crater within Dolomieu. Based on
ground deformation, measured by rapid-static and continuous GPS and an extensometer, seismic data, and lava effusion patterns,
the eruptive period is divided into five stages: 1) slow summit inflation and sporadic seismicity; 2) rapid summit inflation
and a short seismic crisis; 3) rapid flank inflation, onset of summit deflation, sporadic seismicity, accompanied by stable
effusion; 4) flank inflation, coupled with summit deflation, intense seismicity, and increased lava effusion; and finally
5) little deflation, intense shallow seismicity, and the end of lava effusion. We propose a model in which the pre-intrusive
inflation of Stage 1 in the months preceding the eruption was caused by a magma body located near sea level. The magma reservoir
was the source of an intrusion rising under the summit during Stage 2. In Stage 3, the magma ponded at a shallow level in
the edifice while the lateral injection of a radial dike reached the surface on the eastern flank of the basaltic volcano,
causing lava effusion. Pressure decrease in the magmatic plumbing system followed, resulting in upward migration of a collapse
front, forming a subterranean column of debris by faulting and stoping. This caused intense shallow seismicity, increase in
discharge of lava and volcanic tremor at the lateral vent in Stage 4 and, eventually the formation of a pit crater in Stage
5. 相似文献
918.
Christian Tiberius Thomas Pany Bernd Eissfeller Peter Joosten Sandra Verhagen 《GPS Solutions》2002,6(1-2):96-99
In this short contribution it is demonstrated how integer carrier phase cycle ambiguity resolution will perform in near future,
when the US GPS gets modernized and the European Galileo becomes operational. The capability of ambiguity resolution is analyzed
in the context of precise differential positioning over short, medium and long distances. Starting from dual-frequency operation
with GPS at present, particularly augmenting the number of satellites turns out to have beneficial consequences on the capability
of correctly resolving the ambiguities. With a 'double' constellation, on short baselines, the confidence of the integer ambiguity
solution increases to a level of 0.99999999 or beyond.
Electronic Publication 相似文献
919.
Toward micro-scale spatial modeling of gentrification 总被引:1,自引:0,他引:1
David O'Sullivan 《Journal of Geographical Systems》2002,4(3):251-274
A simple preliminary model of gentrification is presented. The model is based on an irregular cellular automaton architecture
drawing on the concept of proximal space, which is well suited to the spatial externalities present in housing markets at
the local scale. The rent gap hypothesis on which the model's cell transition rules are based is discussed. The model's transition
rules are described in detail. Practical difficulties in configuring and initializing the model are described and its typical
behavior reported. Prospects for further development of the model are discussed. The current model structure, while inadequate,
is well suited to further elaboration and the incorporation of other interesting and relevant effects.
Received: 1 November 2001 / Accepted: 12 April 2002
Town centres data were made available by kind permission of the UK Department of the Environment, Transport and the Regions. 相似文献
920.
Use of GPS tracking data from different dual-frequency receiver types (cross-correlating vs. codeless) has revealed satellite-dependent
biases in pseudorange observables P1 (Y-code) and C1 (C/A, Clear Acquisition code). These biases can have a direct effect
on clock estimates, carrier phase bias fixing, and other parameters estimated in GPS data processing. A set of satellite-specific
compensatory pseudorange offsets is calculated, and each is applied to a wee of daily global network analyses in which satlellite,
receiver, atmospheric, and Earth rotation parameters are estimated. Results from these analyses are then compared to those
from corresponding baseline cases in which no biases were applied. There is also some evidence that suggests that the pseudorange
biases differ even among codeless receiver models. Hence, a second set of offsets is computed on a different basis, and compared
with the baseline model in a similar manner. A preliminary examination of C1-P1 variations over time is presented. Finally,
recommendations are made for the use of the calculated offsets, and consideration is given to a future dissemination of updates
to these values as necessary. ? 2001 John Wiley & Sons, Inc. 相似文献