全文获取类型
收费全文 | 1595篇 |
免费 | 420篇 |
国内免费 | 261篇 |
专业分类
测绘学 | 87篇 |
大气科学 | 110篇 |
地球物理 | 888篇 |
地质学 | 548篇 |
海洋学 | 157篇 |
天文学 | 182篇 |
综合类 | 39篇 |
自然地理 | 265篇 |
出版年
2024年 | 2篇 |
2023年 | 8篇 |
2022年 | 24篇 |
2021年 | 36篇 |
2020年 | 44篇 |
2019年 | 65篇 |
2018年 | 43篇 |
2017年 | 68篇 |
2016年 | 54篇 |
2015年 | 71篇 |
2014年 | 89篇 |
2013年 | 78篇 |
2012年 | 46篇 |
2011年 | 66篇 |
2010年 | 79篇 |
2009年 | 93篇 |
2008年 | 123篇 |
2007年 | 88篇 |
2006年 | 154篇 |
2005年 | 117篇 |
2004年 | 106篇 |
2003年 | 69篇 |
2002年 | 85篇 |
2001年 | 75篇 |
2000年 | 61篇 |
1999年 | 65篇 |
1998年 | 53篇 |
1997年 | 35篇 |
1996年 | 67篇 |
1995年 | 53篇 |
1994年 | 42篇 |
1993年 | 42篇 |
1992年 | 26篇 |
1991年 | 20篇 |
1990年 | 28篇 |
1989年 | 19篇 |
1988年 | 24篇 |
1987年 | 9篇 |
1986年 | 6篇 |
1985年 | 3篇 |
1984年 | 2篇 |
1983年 | 4篇 |
1982年 | 2篇 |
1981年 | 5篇 |
1980年 | 5篇 |
1979年 | 3篇 |
1978年 | 10篇 |
1977年 | 2篇 |
1954年 | 7篇 |
排序方式: 共有2276条查询结果,搜索用时 15 毫秒
151.
则木河断裂的现今活动方式及其地形变鉴别标志探讨 总被引:2,自引:0,他引:2
根据地壳形变测量资料,探讨了则木河断裂的现今活动方式及其定性的地形变鉴别标志问题。结果表明:则木河断裂的现今活动具有明显的分段性特征,即以大箐为界分为南北两段,北段以粘滑活动为主,南段以蠕滑活动为主;沿则木河断裂带垂直位移速率空间分布特征的显著差异,可以作为鉴别断裂现今活动方式的标志之一,其位移速率的相对大小,可作为鉴别断裂现今活动方式的一种参考标志 相似文献
152.
本文针对1993年9月中旬以来烟台石英倾斜仪SN向出现的短期异常运用实用化方法对观测数据进行了全面的分析处理。其结果给出,烟台石英倾斜仪异常与1993年12月31日0时29分在东经122°45’,北纬38°10’的Ms4.5级地震有关。 相似文献
153.
The analysis and interpretation of coda waves have received increasing attention since the early seventies. In the past few years interest in this subject has spread worldwide, and the study of high-frequency seismic coda waves has become a very important seismological topic. As a conclusion of the studies accomplished in this time, coda waves are considered the result of scattering processes caused by heterogeneities acting on seismic waves.P andS waves play a particularly important role in this interaction. The process introduces an attenuation which, added to the intrinsic absorption, gives the observed apparent attenuation. Therefore, coda waves constitute a thumbprint left by the heterogeneities on the seismograms. Coda waves offer decisive information about the mechanism of how scattering and attenuation take place. This review describes coda waves in detail, and summarizes the work done in this subject to 1986. The relation between coda waves and attenuation in the context of research on seismic scattering problems is stressed. Particular attention has been given to the application of coda waves to estimate source and medium parameters. The state-of-the-art of the temporal variations of coda wave shape, and the possible use of these variations as an earthquake precursor also are presented. Care has been taken to introduce the statistical models used to deal with the heterogeneities responsible for scattering. 相似文献
154.
The formal solutions of displacement field to the problem of elastic wave scattering and diffraction due to an infinitely long rigid cylinder embedded in an infinite elastic medium by an impulsive point source have been obtained in the integral form. The integrals for the reflected and the diffracted waves both in the shadow zone and in the illuminated zone are evaluated asymptotically for the early time motion by the Reisdue-Cagniard method and the Saddle-point-Cagniard method.Numerical results of the diffractedP, S andPS waves at a fixed circum-distance from the surface of the rigid cylinder show noticeably that (1) the energy partition for the diffractedS wave is small in comparison with that for the diffractedP wave, (2) the wave form of the diffractedS wave is broader and more diffused than that of the diffractedP wave, (3) the direction of the radial motions of the diffractedP andS waves varies as a function of the observational point, and (4) the energy partition for the diffractedP wave is much smaller than that for the direct or the reflectedP waves.This paper has been presented at the 46th Annual International Meeting of Society of Exploration Geophysicists in Houston, Texas, Oct. 28, 1976. 相似文献
155.
C. O. Oluwafemi 《Pure and Applied Geophysics》1983,121(5-6):1065-1076
Solar, sky, and aureole radiance data from Kensington, Australia, and Lagos, Nigeria, are analysed. The values of the aerosol
optical thickness at Lagos are comparable to measured values elsewhere in the subregion (Abidjan) under light haze. The values
at Kensington are close to those of the “background aerosol.” Identical and anomalous values of aerosol optical thickness
occurred at 1.67 μm at both stations as less than 15% of the values can be accounted for by aerosols. The high optical depths
are therefore explained in terms of absorption, possibly mainly by CO2 (59–65%) and, to a lesser extent, by H2O (20–26%). Following correction for molecular multiple scattering, the aerosol scattering phase function increases substantially
at 0.5 μm in Kensington and decreases considerably at 0.76 μm in Lagos when compared to the uncorrected function, confirming
the relative fineness of the Kensington aerosol. The Lagos aerosol size distribution for moderately dusty air is reasonably
bimodally log-normal with modal radiusr
m=0.49 μm (1.36 μm) for the moder≤1 μm (r>1 μm). The Kensington aerosol resembles one withr
m=0.05 μm forr<1 μm. There the Born approximation appears appropriate, and the weighted mean square radiusp
2=0.13 μm2. In the near forward direction the aerosol scattering phase funciton for Lagos resembles Deirmendjian’s simulations for a
silicate-L haze and, for Kensington, a silicate-H haze. 相似文献
156.
157.
结合安徽省高速公路建设工程实例,介绍瞬态瑞雷面波勘探技术在公路工程地质勘察中的应用,解决沿线高边坡、深路堑、桥梁、隧道进出口的岩土分层,给出基岩风化分带等工程地质问题,省时、省力,取得了良好的经济效益和环境效益. 相似文献
158.
Sebastian Hinsken Kamil Ustaszewski Andreas Wetzel 《International Journal of Earth Sciences》2007,96(6):979-1002
Eocene to Early Oligocene syn-rift deposits of the southern Upper Rhine Graben (URG) accumulated in restricted environments.
Sedimentation was controlled by local clastic supply from the graben flanks, as well as by strong intra-basinal variations
in accommodation space due to differential tectonic subsidence, that in turn led to pronounced lateral variations in depositional
environment. Three large-scale cycles of intensified evaporite sedimentation were interrupted by temporary changes towards
brackish or freshwater conditions. They form three major base level cycles that can be traced throughout the basin, each of
them representing a stratigraphic sub-unit. A relatively constant amount of horizontal extension (ΔL) in the range of 4–5 km has been estimated for the URG from numerous cross-sections. The width of the rift (L
f
), however, varies between 35 and more than 60 km, resulting in a variable crustal stretching factor between the bounding
masterfaults. Apart from block tilting, tectonic subsidence was, therefore, largely controlled by changes in the initial rift
width (L
0). The along-strike variations of the graben width are responsible for the development of a deep, trough-like evaporite basin
(Potash Basin) in the narrowest part of the southern URG, adjacent to shallow areas in the wider parts of the rift such as
the Colmar Swell in the north and the Rhine Bresse Transfer Zone that delimits the URG to the south. Under a constant amount
of extension, the along-strike variation in rift width is the principal factor controlling depo-centre development in extensional
basins. 相似文献
159.
Allen P. Nutman Vickie C. Bennett Clark R. L. Friend Kenji Horie Hiroshi Hidaka 《Contributions to Mineralogy and Petrology》2007,154(4):385-408
The Eoarchaean (>3,600 Ma) Itsaq Gneiss Complex of southern West Greenland is dominated by polyphase orthogneisses with a
complex Archaean tectonothermal history. Some of the orthogneisses have c. 3,850 Ma zircons, and they vary from rare single
phase metatonalites to more common complexly banded migmatites. This is due to heterogeneous strain, in situ anatexis and
granitic veining superimposed during younger tectonothermal events. In the single-phase tonalites with c. 3,850 Ma zircon,
oscillatory-zoned prismatic zircon is all 3,850 Ma old, but shows patchy ancient loss of radiogenic Pb. SHRIMP spot analyses
and laser ablation ICP-MS depth profiling show that thin (usually < 10 μm) younger (3,660–3,590 Ma and Neoarchaean) shells
of lower Th/U metamorphic zircon are present on these 3,850 Ma zircons. Several samples with this simple zircon population
occur on islands near Akilia. In contrast, migmatites usually contain more complex zircon populations, with often more than
one generation of igneous zircon present. Additional zircon dating of banded gneisses across the Complex shows that samples
with c. 3,850 Ma igneous zircon are not just a phenomenon restricted to Akilia and adjacent islands. For example, migmatites
from Itilleq (c. 65 km from Akilia) contain variable amounts of oscillatory-zoned 3,850 Ma and 3,650 Ma zircon, interpreted,
respectively, as the rock age and the time of crustal melting under Eoarchaean metamorphism. With only 110–140 ppm Zr in the
tonalites and likely magmatic temperatures of >850°C, zircon solubility–melt composition relationships show that they were
only one-third saturated in zircon. Any zircon entrained in the precursor magmas would thus have been highly soluble. Combined
with the cathodoluminesence imaging, this demonstrates that the c. 3,850 Ma oscillatory zoned zircon crystallised out of the
melt and hence gives a magmatic age. Thus the rare well-preserved tonalites and palaeosome in migmatites testify that c. 3,850 Ma
quartzo–feldspathic rocks are a widespread (but probably minor) component in the Itsaq Gneiss Complex. C. 3,850 Ma zircon
with negative Eu anomalies (showing growth in felsic systems) also occurs as detrital grains in rare c. 3,800 Ma metaquartzites
and as inherited grains in some 3,660 Ma granites (sensu stricto). These demonstrate that still more c. 3,850 Ma rocks were present, but were recycled into Eoarchaean sediments and crustally
derived granites. The major and trace element characteristics (e.g. LREE enrichment, HREE depletion, low MgO) of the best-preserved
c. 3,850 Ma rocks are typical of Archaean TTG suites, and thus argue for crust formation processes involving important contributions
from melting of hydrated mafic crust to the earliest Archaean. Five c. 3,850 Ma tonalites were selected as the best preserved
on the basis of field criteria and zircon petrology. Four of these samples have overlapping initial ɛNd (3,850 Ma) values from +2.9 to +3.6± 0.5, with the fourth having a slightly lower value of +0.6. These data provide additional
evidence for a markedly LREE-depleted early terrestrial mantle reservoir. The role of c. 3,850 Ma crust should be considered
in interpreting isotope signatures of the younger (3,800–3,600 Ma) rocks of the Itsaq Gneiss Complex.
Electronic supplementary material The online version of this article (doi:) contains supplementary material, which is available to authorized users. 相似文献
160.