全文获取类型
收费全文 | 516篇 |
免费 | 11篇 |
国内免费 | 4篇 |
专业分类
测绘学 | 17篇 |
大气科学 | 57篇 |
地球物理 | 105篇 |
地质学 | 169篇 |
海洋学 | 49篇 |
天文学 | 77篇 |
综合类 | 2篇 |
自然地理 | 55篇 |
出版年
2024年 | 4篇 |
2021年 | 5篇 |
2020年 | 4篇 |
2019年 | 7篇 |
2018年 | 18篇 |
2017年 | 7篇 |
2016年 | 14篇 |
2015年 | 12篇 |
2014年 | 19篇 |
2013年 | 24篇 |
2012年 | 24篇 |
2011年 | 27篇 |
2010年 | 9篇 |
2009年 | 17篇 |
2008年 | 12篇 |
2007年 | 17篇 |
2006年 | 27篇 |
2005年 | 17篇 |
2004年 | 11篇 |
2003年 | 6篇 |
2002年 | 30篇 |
2001年 | 17篇 |
2000年 | 7篇 |
1999年 | 9篇 |
1998年 | 17篇 |
1996年 | 6篇 |
1995年 | 6篇 |
1994年 | 7篇 |
1993年 | 6篇 |
1992年 | 9篇 |
1991年 | 11篇 |
1990年 | 7篇 |
1989年 | 4篇 |
1988年 | 9篇 |
1986年 | 6篇 |
1985年 | 6篇 |
1984年 | 11篇 |
1983年 | 4篇 |
1981年 | 6篇 |
1979年 | 3篇 |
1978年 | 3篇 |
1977年 | 4篇 |
1976年 | 4篇 |
1975年 | 4篇 |
1973年 | 5篇 |
1970年 | 4篇 |
1962年 | 3篇 |
1961年 | 3篇 |
1960年 | 4篇 |
1955年 | 3篇 |
排序方式: 共有531条查询结果,搜索用时 796 毫秒
21.
A 39-km-long deep seismic reflection profile recorded during two field campaigns in 1996 and 2002 provides a first detailed image of the deep crust at the eastern margin of the Eastern Alps (Austria). The ESE–WNW-trending, low-fold seismic line crosses Austroalpine basement units and extends approximately from 20 km west of the Penninic window group of Rechnitz to 60 km SSE of the Alpine thrust front.The explosive-source seismic data reveals a transparent shallow crust down to 5 km depth, a complexly reflective upper crust and a highly reflective lowermost crust. The upper crust is dominated by three prominent west-dipping packages of high-amplitude subparallel reflections. The upper two of these prominent packages commence at the eastern end of the profile at about 5 and 10 km depth and are interpreted as low-angle normal shear zones related to the Miocene exhumation of the Rechnitz metamorphic core complex. In the western portion of the upper crust, east-dipping and less significant reflections prevail. The lowermost package of these reflections is suggested to represent the overall top of the European crystalline basement.Along the western portion of the line, the lower crust is characterised by a 6–8-km-thick band of high-amplitude reflection lamellae, typically observed in extensional provinces. The Moho can be clearly defined at the base of this band, at approximately 32.5 km depth. Due to insufficient signal penetration, outstanding reflections are missing in the central and eastern portion of the lower crust. We speculate that the result of accompanying gravity measurements and lower crustal sporadic reflections can be interpreted as an indication for a shallower Moho in the east, preferable at about 30.5 km depth.The high reflectivity of the lowermost part of the lower crust and prominent reflection packages in the upper crust, the latter interpreted to represent broad extensional mylonite zones, emphasises the latest extensional processes in accordance with eastward extrusion. 相似文献
22.
Imaging the Dead Sea Transform with scattered seismic waves 总被引:2,自引:0,他引:2
23.
24.
25.
26.
Kenneth B. Raposa Scott Lerberg Craig Cornu John Fear Nina Garfield Christopher Peter Robin L.J. Weber Gregg Moore David Burdick Michelle Dionne 《Estuaries and Coasts》2018,41(1):36-51
Evaluations of tidal wetland restoration efforts suffer from a lack of appropriate reference sites and standardized methods among projects. To help address these issues, the National Estuarine Research Reserve System (NERRS) and the NOAA Restoration Center engaged in a partnership to monitor ecological responses and evaluate 17 tidal wetland restoration projects associated with five reserves. The goals of this study were to (1) determine the level of restoration achieved at each project using the restoration performance index (RPI), which compares change in parameters over time between reference and restoration sites, (2) compare hydrologic and excavation restoration projects using the RPI, (3) identify key indicator parameters for assessing restoration effectiveness, and (4) evaluate the value of the NERRS as reference sites for local restoration projects. We found that the RPI, modified for this study, was an effective tool for evaluating relative differences in restoration performance; most projects achieved an intermediate level of restoration from 2008 to 2010, and two sites became very similar to their paired reference sites, indicating that the restoration efforts were highly effective. There were no differences in RPI scores between hydrologic and excavation restoration project types. Two abiotic parameters (marsh platform elevation and groundwater level) were significantly correlated with vegetation community structure and thus can potentially influence restoration performance. Our results highlight the value of the NERRS as reference sites for assessing tidal wetland restoration projects and provide improved guidance for scientists and restoration practitioners by highlighting the RPI as a trajectory analysis tool and identifying key monitoring parameters. 相似文献
27.
Prof. Dr. K. Hinz Dr. J. Fritsch Dr. E. H. K. Kempter Mr. A. Manaf Mohammad Dr. J. Meyer Mr. D. Mohamed Dipl. Geophys. H. Vosberg Dipl. Ing. J. Weber Mr. J. Benavidez 《International Journal of Earth Sciences》1989,78(3):705-730
Widely accepted plate tectonic models suggest that an inactive subduction zone lies along the north-west continental margin of Sabah. In contrast, interpretation of reflection seismic data acquired by BGR shows an autochthonous continental terrane comprising an Oligocene to Early Miocene carbonate platform being progressively overthrust by an allochthonous rock complex. Progressive compression resulted in the development of four structural zones: Imbricated thrust sheets (Zone III); two thrust sheet systems one on top of the other (Zone IV); a complex zone with multiphase deformation (Zone V); and piercement ridges (Zone VI).
Zusammenfassung Nach herkömmlichen plattentektonischen Vorstellungen soll eine inaktive Subduktionszone am nordwestlichen Kontinentalrand von Sabah liegen. Reflexionsseismische Meßdaten der BGR zeigen jedoch, daß hier autochthone kontinentale Kruste mit einer oligozänen-frühmiozänen Karbonatplattform progressiv von einem allochthonen Gesteinsverband überschoben wird. Fortschreitender Zusammenschub seit dem frühen Miozän führte zur Anlage von vier Deformationszonen: Tekonische Schuppen (Zone III); zwei übereinander geschobene Verschuppungssysteme (Zone IV); Gürtel mit mehrphasiger Deformation (Zone V) und Durchspießungsstrukturen (Zone VI).
Résumé Les modèles géodynamiques que l'on admet habituellement comportent une zone de subduction inactive le long de la marge continentale nord-occidentale de Sabah. Toutefois, des mesures de sismique-réflexion exécutées par le BGR font apparaître qu'à cet endroit, une croûte continentale autochtone, comportant une plateforme carbonatée oligocène à éomiocène, est chevauchée progressivement par un complexe allochtone. La compression, qui s'est manifestée progressivement depuis le Miocène inférieur, a engendré quatre zones structurales: un ensemble d'écailles tectoniques (zone III); deux systèmes de lames tectoniques charriés l'un sur l'autre (zone IV); une zone complexe à déformation multiphasée (zone V); des structures d'extrusion tectonique (zone VI).
, - Sabah'a. , - . 4-? : ( 3), ( 4) ( 5) ( 6).相似文献
28.
Spherical harmonic expansions of the geopotential are frequently used for modelling the earth’s gravity field. Degree and
order of recently available models go up to 360, corresponding to a resolution of about50 km. Thus, the high degree potential coefficients can be verified nowadays even by locally distributed sets of terrestrial gravity
anomalies. These verifications are important when combining the short wavelength model impact, e.g. for regional geoid determinations
by means of collocation solutions. A method based on integral formulae is presented, enabling the improvement of geopotential
models with respect to non-global distributed gravity anomalies. To illustrate the foregoing, geoid computations are carried
out for the area of Iran, introducing theGPM2 geopotential model in combination with available regional gravity data. The accuracy of the geoid determination is estimated
from a comparison with Doppler and levelling data to ±1.4m. 相似文献
29.
30.
G. -R. Weber 《Theoretical and Applied Climatology》1990,41(1-2):1-9
Summary The annual amount of sunshine during the 37-year period from 1951 through 1987 has been analyzed for 54 stations in the Federal Republic of Germany. Sunshine generally decreased during this period over the eastern half of the country and in the central German hills. For some stations, the loss amounts to more than 300 hours per year, more than 18% of total received sunshine. Mountain tops in the central German hills show the greatest decline; this may result from increased cyclonic episodes over Central Europe. The decrease in sunshine over central and northeastern Germany was not accompanied by increased precipitation, or by number of days of precipitation.With 5 Figures 相似文献