全文获取类型
收费全文 | 182篇 |
免费 | 5篇 |
国内免费 | 1篇 |
专业分类
测绘学 | 1篇 |
大气科学 | 19篇 |
地球物理 | 47篇 |
地质学 | 64篇 |
海洋学 | 21篇 |
天文学 | 19篇 |
综合类 | 2篇 |
自然地理 | 15篇 |
出版年
2020年 | 2篇 |
2019年 | 2篇 |
2018年 | 2篇 |
2016年 | 4篇 |
2015年 | 2篇 |
2014年 | 5篇 |
2013年 | 7篇 |
2012年 | 9篇 |
2011年 | 7篇 |
2010年 | 9篇 |
2009年 | 7篇 |
2008年 | 8篇 |
2007年 | 4篇 |
2006年 | 7篇 |
2005年 | 6篇 |
2004年 | 6篇 |
2003年 | 5篇 |
2002年 | 8篇 |
2001年 | 3篇 |
2000年 | 2篇 |
1999年 | 3篇 |
1998年 | 2篇 |
1996年 | 3篇 |
1995年 | 1篇 |
1994年 | 3篇 |
1993年 | 2篇 |
1992年 | 2篇 |
1991年 | 5篇 |
1990年 | 2篇 |
1988年 | 1篇 |
1987年 | 2篇 |
1986年 | 3篇 |
1985年 | 5篇 |
1984年 | 7篇 |
1983年 | 5篇 |
1982年 | 4篇 |
1981年 | 4篇 |
1980年 | 1篇 |
1979年 | 5篇 |
1977年 | 1篇 |
1976年 | 2篇 |
1975年 | 3篇 |
1974年 | 1篇 |
1973年 | 4篇 |
1972年 | 1篇 |
1971年 | 1篇 |
1970年 | 2篇 |
1961年 | 2篇 |
1956年 | 1篇 |
1928年 | 1篇 |
排序方式: 共有188条查询结果,搜索用时 15 毫秒
71.
Thierry Dumont Jean-Daniel Champagnac Christian Crouzet Philippe Rochat 《Swiss Journal of Geoscience》2008,101(1):89-110
Three-dimensional modelling tools are used with structural and palaeomagnetic analysis to constrain the tectonic history of part of the Dauphiné zone (external Western Alps). Four compressive events are identified, three of them being older than the latest Oligocene. Deformation D1 consists of W–SW directed folds in the Mesozoic cover of the study area. This event, better recorded in the central and southern Pelvoux massif, could be of Eocene age or older. Deformation D2 induced N-NW-oriented basement thrusting and affected the whole southern Dauphiné basement massifs south of the study area. The main compressional event in the study area (D3) was WNW oriented and occurred before 24 Ma under a thick tectonic load probably of Penninic nappes. The D2-D3 shift corresponds to a rapid transition from northward propagation of the Alpine collision directly driven by Africa-Europe convergence, to the onset of westward escape into the Western Alpine arc. This Oligocene change in the collisional regime is recorded in the whole Alpine realm, and led to the activation of the Insubric line. The last event (D4) is late Miocene in age and coeval with the final uplift of the Grandes Rousses and Belledonne external massifs. It produced strike-slip faulting and local rotations that significantly deformed earlier Alpine folds and thrusts, Tethyan fault blocks and Hercynian structures. 3D modelling of an initially horizontal surface, the interface between basement and Mesozoic cover, highlights large-scale basement involved asymmetric folding that is also detected using structural analysis. Both, Jurassic block faulting and basement fold-and-thrust shortening were strongly dependent on the orientation of Tethyan extension and Alpine shortening relative to the late Hercynian fabric. The latter’s reactivation in response to oblique Jurassic extension produced an en-échelon syn-rift fault pattern, best developed in the western, strongly foliated basement units. Its Alpine reactivation occurred with maximum efficiency during the early stages of lateral escape, with tectonic transport in the overlying units being sub-perpendicular to it. 相似文献
72.
Thi Phuong Quynh Le Viet Nga Dao Emma Rochelle‐Newall Josette Garnier XiXi Lu Gilles Billen Thi Thuy Duong Cuong Tu Ho Henri Etcheber Thi Mai Huong Nguyen Thi Bich Ngoc Nguyen Bich Thuy Nguyen Nhu Da Le Quoc Long Pham 《地球表面变化过程与地形》2017,42(9):1329-1341
Riverine transport of organic carbon from terrestrial ecosystems to the oceans plays an important role in the global carbon cycle. The Red River is located in Southeast Asia where river discharge, sediment loads and fluxes of elements (carbon, nitrogen and phosphorus) associated with suspended solids have been dramatically altered over past decades as a result of reservoir impoundment and land use, population, and climate change. Dissolved organic carbon (DOC) and particulate organic carbon (POC) concentrations were measured monthly at four stations of the Red River system from January 2008 to December 2010. The results reveal that POC changed synchronically with total suspended solids (TSS) concentration and with the river discharge, whereas no clear trend was observed for DOC concentration. The mean value of total organic carbon (TOC = DOC + POC) flux in the delta of the Red River was 31.5 × 1013 ± 4.0 × 1013 MgC.yr?1 (range 27.9–35.8 × 1013 MgC.yr?1 which leads to a specific TOC flux of 2012 ± 255 kgC.km?2.yr?1 during this 2008–2010 period. About 80% of the TOC flux was transferred to the estuary during the rainy season as a consequence of the higher river water discharge. The high mean value of the POC:Chl‐a ratio (1585 ± 870 mgC.mgChl‐a?1) and the moderate C:N ratio (7.3 ± 0.1) in the water column system suggest that organic carbon in the Red River system is mainly derived from erosion and soil leaching in the basin. The effect of two new dam impoundments in the Red River was also observable with lower TOC fluxes in 2010 compared with 2008. Copyright © 2017 John Wiley & Sons, Ltd. 相似文献
73.
Julien Charreau Amandine Sartgou Dimitri Saint‐Carlier Jrme Lav Pierre‐Henri Blard Stphane Dominguez Sheng Li Wang Gang Rao 《地学学报》2020,32(1):89-96
In this study, we reconstruct the Miocene to Quaternary shortening history across the Qiulitag anticline, a complex fault‐bend fold located in southern Tianshan. We studied the Yaha and Kuche sections, where we combined surface structural measurements and seismic imaging to model the stratigraphic horizons. The history of folding was reconstructed based on magnetostratigraphic analyses and eight cosmogenic burial ages in Kuche. Pleistocene deformation rates were also quantified in Yaha based on a deformed fluvial terrace that we dated to ~67 ka using a cosmogenic depth profile. Our results suggest that the fold grew at a mean slip rate of 0.9–1.3 mm/a in both sections but accelerated to ~2.5 mm/a during the Pleistocene in Kuche. These results support a migration of the deformation towards the basin during the Pleistocene and suggest that most of the present deformation in the Tianshan is accommodated across the external structures of the range. 相似文献
74.
R. Dumont G. Soulié M. Rapaport F. Sánchez-Martinez 《Astrophysics and Space Science》1970,9(1):175-180
Observations have been selected in Tenerife Zodiacal Light Data, which make it possible to separate the diffuse galactic light from other components. Far from the Milky Way (30°|b|60°) the diffuse galactic light shows a decreasing slope which cannot exceed –0.3S
10 vis. per degree of galactic latitude, and is probably a very weak component of the total extraterrestrial light. 相似文献
75.
76.
Si iv, C iv, and O vi resonance lines have been measured above quiet and active solar regions from both pointed OSO-8 instruments. From calibrated profiles, optical depths are computed with three different methods. All three methods provide evidence that the opacity above faculae is lower than above the quiet Sun. From lower and upper limits of the opacity, we derive limits of the electron density. Our first method assumes only that the source function is constant without any geometrical constraint. We find higher densities above faculae than above quiet regions (about a factor 10). A second method allows us to compute the density, temperature gradient and thickness of a plane-parallel model, for active and quiet Sun. Electron densities agree with those of the first method but they lie in the lower range of values previously determined from Skylab. This result can be explained by the moderate level activity of the observed faculae. Appendices give relevant elements of transfer theory and newly computed values of collisional rates. 相似文献
77.
Di Bernardino Annalisa Iannarelli Anna Maria Diémoz Henri Casadio Stefano Cacciani Marco Siani Anna Maria 《Theoretical and Applied Climatology》2022,147(1-2):291-305
Theoretical and Applied Climatology - The extreme temperature events are a concern in recent years due to climate variability particularly in India as there is an increase in the temperature... 相似文献
78.
Gilbert Mille Jan Yu Chen Henri Dou Edgar Azoulay Maryse Colin Jean-Claude Bertrand 《Marine environmental research》1985,17(1):65-80
Coastal Mediterranean sediments highly polluted by refinery effluents have been studied for their hydrocarbon content and bacterial activity. The study has taken into account both the distance from the refinery and depth of sampling. Very high hydrocarbon concentrations have been found (1–250 g/kg dry sediment). Micro-organisms in the sediments have a high bacterial activity and a good correlation exists between hydrocarbon concentrations and bacteria able to use these substrates as a carbon and energy source. 相似文献
79.
Hydrogeochemical modeling of organo-metallic colloids in the Nsimi experimental watershed,South Cameroon 总被引:1,自引:0,他引:1
M. Sekhar Jean-Jacques Braun K. V. Hayagreeva Rao Laurent Ruiz Henri Robain Jérôme Viers Jules Rémy Ndam Bernard Dupré 《Environmental Geology》2008,54(4):831-841
This paper presents a hydrogeochemical modeling code HYDROS, which combines the multi-component transport model with equilibrium
speciation module MINTEQA2. The processes of adsorption, aqueous speciation and mineral precipitation/dissolution are represented
in the model. The numerical model uses a sequential iterative approach for solving the solute transport and the equilibrium
geochemistry modules. Further the transport part is solved using an operator split approach wherein a finite volume method
is used for solving the advective equations while a classical finite difference method is employed for solving the dispersive
equations. The model performance is evaluated by comparing it with MINTOX for a literature problem. HYDROS is then applied
to the case study of the transfer of transition metals with organic colloids in the swamp groundwater system of the experimental
Nsimi watershed, representative of the humid tropical ecosystem of the South Cameroon Plateau. Field observations at the site
swamp system suggest that the carbon is mainly transferred as organic colloids (i.e., dissolved organic carbon) produced by
the slow biodegradation of the swamp organic matter. Using HYDROS, the behaviour of Al(III) and Fe(III) elements in the base
flow system is simulated during inter rain events of a short rainy season (May–June 1996). The elemental time-series for Al,
Fe, Cl, pH compare well with the simulation results. The colloids are found to have a strong impact on the mobilization and
transfer of Al(III) and Fe(III), which are considered to have low mobility in weathering environment. 相似文献
80.