收费全文 | 181篇 |
免费 | 4篇 |
国内免费 | 4篇 |
测绘学 | 2篇 |
大气科学 | 26篇 |
地球物理 | 33篇 |
地质学 | 86篇 |
海洋学 | 12篇 |
天文学 | 16篇 |
综合类 | 1篇 |
自然地理 | 13篇 |
2022年 | 8篇 |
2021年 | 4篇 |
2020年 | 5篇 |
2019年 | 1篇 |
2018年 | 4篇 |
2017年 | 4篇 |
2016年 | 8篇 |
2015年 | 8篇 |
2014年 | 16篇 |
2013年 | 9篇 |
2012年 | 6篇 |
2011年 | 11篇 |
2010年 | 17篇 |
2009年 | 11篇 |
2008年 | 15篇 |
2007年 | 8篇 |
2006年 | 9篇 |
2005年 | 6篇 |
2004年 | 3篇 |
2003年 | 2篇 |
2002年 | 1篇 |
2001年 | 1篇 |
2000年 | 3篇 |
1999年 | 3篇 |
1998年 | 3篇 |
1997年 | 2篇 |
1996年 | 1篇 |
1995年 | 3篇 |
1992年 | 1篇 |
1991年 | 1篇 |
1987年 | 1篇 |
1979年 | 1篇 |
1978年 | 1篇 |
1974年 | 4篇 |
1973年 | 1篇 |
1970年 | 1篇 |
1969年 | 3篇 |
1965年 | 1篇 |
1964年 | 1篇 |
1956年 | 1篇 |
Die Verteilung von Fe2+ und Fe3+ in eisenhaltigen Turmalinen: Eine Mössbauer-Untersuchung
Zusammenfassung Mössbauer-Spektren von fünf eisenhaltigen Turmalinen wurden gemessen und analysiert. Das Verhältnis Fe2+/Fe3+ und die Eisenverteilung konnten mit Hilfe von zwei gut identifizierten Turmalin-Kristallen von Mexiko und Madagascar für die Y-und Z-Lagen aller Exemplare bestimmt werden. Zweiwertiges sowie dreiwertiges Eisen findet sich sowohl in der Z-als auch in der Y-Lage. Da sich die Y-und Z-Oktaeder in einer gemeinsamen Kante treffen, wird diese Beobachtung als chemische Antwort des Kristalles auf die erforderte Größenanpassung der Y-und Z-Oktaeder während seines Wachstums erklärt. Die Abwesenheit der festen Lösung zwischen Dravit und Elbait kann somit erklärt werden.
With 4 Figures 相似文献
Summary A white gel-like mineral containing more than 90% moisture was found in a quarry near Gumpoldskirchen (Lower Austria). The mineral had been formed recently in gaps and cavities of a fissure system in the Triassic Main Dolomite.Airdried, the jelly mineral turns into a paper-like skin (rockmilk) and can be recrystallised to a white earthy crust (rockflour).The chemical analysis, the X-ray diffraction and electron diffraction investigation show that the mineral is calcite, even it contains high amounts of water. The electronmicroscopical investigations explain the properties of this peculiar formation of the mineral. If the mineral is containing water, the filiform crystallites of calcite 500 Å of diameter are completely disorderd. The water is bound adsorptively in the framework of calcite crystallites. During the loss of water the filiform calcite crystalls are ordered more or less parallel to each other.The name protocalcite is proposed for this variety of calcite, which is containing variable amounts of water (CaCO3+xH2O).
Mit 9 Textabbildungen
Herrn Professor Dr.F. Machatschki zum 70. Geburtstag gewidmet. 相似文献
- 1. One of the reasons for the soft-sediment deformation might have been the relatively low cohesive strength of the predominantly smectitic sediment covering a gentle slope similar to the actual landscape.
2. On such a surface, the down-slope gravitational component of the mud-blanket might easily have been sufficient to overcome its cohesive strength.
3. Frost action traceable in the studied formations might also have contributed to the observed deformation, particularly along the eroded top of the Late Miocene sediments.
Combined evidence from field observations and laboratory analyses support the idea that liquefaction–fluidization was of prime importance in bringing about the observed structures. In conclusion two alternative Quaternary/Holocene scenarios are proposed, which might have resulted in the unusual behaviour of the sediments/paleosols. One is a seismic event, the other is the combined effect of freeze–thaw cycles and of the sloping foothill position, which might have resulted in episodic downslope transport and the associated deformation of the eroded soil material when its water content surpassed a certain threshold. We accept that the anomalous abundance of soft-sediment deformation in this marginal position may be causally related to paleo-earthquakes, but the obvious complexity of the phenomenon requires caution. In case the proposed scenarios would not have been alternatives but acted simultaneously, the analysed phenomena were to be interpreted as the joint results of tectonics and climate change. 相似文献
Shales play important roles in various civil, energy and environmental engineering applications. Shales are categorized as poroelastic materials due to their tight and very stiff structure, and reliable poroelastic properties are required when dealing with shales. This paper presents simple procedures to determine the poroelastic properties of rocks using oedometer and triaxial consolidation tests. The procedures, which avoid the difficulty to perform determination of the unjacketed bulk modulus of the rock minerals, are demonstrated on a North Sea shale. The experimentally obtained Biot coefficient α and the drained bulk modulus K of the shale range from 0.95 to 0.99, and from 0.17 to 2.00 GPa, respectively. The Biot coefficient α and the drained bulk modulus K values determined from the oedometer and triaxial tests are compared and show good agreement and consistency between the two test procedures. The Skempton’s coefficient B-value of the triaxial samples was also experimentally measured prior to the triaxial consolidation tests. The theoretically predicted B-value varies from 0.81 to 0.96 which is, on the average, only about 10% higher than the experimentally obtained B-value which range from 0.80 to 0.85.
相似文献