全文获取类型
收费全文 | 645篇 |
免费 | 12篇 |
国内免费 | 4篇 |
专业分类
测绘学 | 9篇 |
大气科学 | 67篇 |
地球物理 | 127篇 |
地质学 | 284篇 |
海洋学 | 36篇 |
天文学 | 109篇 |
综合类 | 4篇 |
自然地理 | 25篇 |
出版年
2019年 | 7篇 |
2018年 | 11篇 |
2017年 | 7篇 |
2016年 | 17篇 |
2015年 | 9篇 |
2014年 | 16篇 |
2013年 | 28篇 |
2012年 | 11篇 |
2011年 | 27篇 |
2010年 | 23篇 |
2009年 | 42篇 |
2008年 | 18篇 |
2007年 | 25篇 |
2006年 | 18篇 |
2005年 | 24篇 |
2004年 | 19篇 |
2003年 | 18篇 |
2002年 | 14篇 |
2001年 | 6篇 |
2000年 | 13篇 |
1999年 | 8篇 |
1997年 | 11篇 |
1996年 | 6篇 |
1995年 | 6篇 |
1994年 | 10篇 |
1993年 | 9篇 |
1992年 | 6篇 |
1990年 | 5篇 |
1987年 | 7篇 |
1986年 | 6篇 |
1985年 | 8篇 |
1984年 | 9篇 |
1982年 | 16篇 |
1981年 | 10篇 |
1980年 | 14篇 |
1979年 | 5篇 |
1978年 | 7篇 |
1977年 | 8篇 |
1976年 | 9篇 |
1975年 | 7篇 |
1974年 | 9篇 |
1973年 | 9篇 |
1972年 | 5篇 |
1971年 | 9篇 |
1970年 | 5篇 |
1968年 | 6篇 |
1967年 | 7篇 |
1966年 | 5篇 |
1959年 | 7篇 |
1954年 | 6篇 |
排序方式: 共有661条查询结果,搜索用时 15 毫秒
61.
Detailed facies analysis of hyaloclastites and associated lavas from eight table mountains and similar "hyaloclastite volcanoes"
in the Icelandic rift zone contradict a rapid and continuous, "monogenetic", entirely subglacial evolution of most volcanoes
studied. The majority of the exposed hyaloclastite deposits formed in large, stable lakes as indicated by widespread, up to
300-m-thick, continuous sections of deep water, shallow water and emergent facies. Salient features include extensively layered
or bedded successions comprising mainly debris flow deposits, turbidites, base surge and fallout deposits consisting of texturally
and compositionally variable, slightly altered hyaloclastites, as well as sheet and pillow lavas. In contrast, chaotic assemblages
of coarser-grained, more poorly sorted and more strongly palagonitized hyaloclastite tuffs and breccias, as well as scoria
and lava are interpreted to have formed under sub- or englacial conditions in small, chimney-like ice cavities or ice-bound
lakes. Irregularly shaped and erratically arranged hyaloclastite bodies produced at variable water levels appear to have resulted
mainly from rapid changes of the eruptive environment due to repeated build-up and drainage of ice-bound lakes as well as
the restricted space between the ice walls. We distinguish a "deep water" facies formed during high water levels of the lake,
a hydroclastic shallow water and emergent facies (leakage of the lake or growth of the volcano above the water surface). Our
model implies the temporary existence of large, stable lakes in Iceland probably formed by climatically induced ice melting.
The highly complex edifices of many table mountains and similar volcanoes were constructed during several eruptive periods
in changing environments characterized by contrasting volcanic and sedimentary processes.
Received: 10 June 1997 / Accepted: 28 July 1998 相似文献
62.
Werner Borchert 《Contributions to Mineralogy and Petrology》1948,1(2-3):203-212
Zusammenfassung Die Analyse der Verfärbungserscheinungen bei Bestrahlung von Steinsalz mit Röntgenstrahlen führt auf die Entstehung einer uneinheitlichen, optisch nicht trennbarenF-Bande mit einem ausgeprägten Absorptionsmaximum bei 465 m. Die unter den Bedingungen: unbehandeltes Kristallmaterial, Zimmertemperatur, schwaches diffuses Licht, durchgeführte Bestrahlung ergibt stabileF-,. metastabileF
*- und instabileF-Zentren, die alle derF-Bande angehören. DieF
*-Zentren sind während der Einstrahlung stabil, während sich dieF -Zentren proportional ihrer Anzahl umwandeln.Für die Umwandlung derF
*-Zentren nach Aufhören der Einstrahlung nehmen wir den Übergang inF
2-Zentren, die früher schon bei optischer Erregung durch Einstrahlung in die Hauptbande gefunden wurden, an. Die Entstehung dieser Zentren bei Erregung wird durch die Erweiterung des absteigenden Astes derF-Bande nach längeren Wellenlängen hin angezeigt.DieF-Zentren gehen während und nach der Bestrahlung inF
3-Zentren über, die durch das Auftreten einer Nebenbande mit einem Absorptionsmaximum bei etwa 720 m gekennzeichnet ist. Dieser Vorgang wird besonders deutlich durch das Ansteigen derF
3-Bande trotz Aufhörens der Einstrahlung. Die bei derF-Bande gefundene Aufteilung in unterschiedlich stabile Zentren ist auch auf die anderen Banden anzuwenden.Die hier entwickelten Vorstellungen über die Bildung und Umbildung der verschiedenen Zentrenarten stehen in Übereinstimmung mit den gemessenen Anklingungs- und Abklingungskurven. 相似文献
63.
64.
With the help of a model atmosphere of the Sun we evaluate the pole-equator difference in flux (as measured by Dicke and Goldenberg) assuming the following type of pole-equator temperature difference (T=T
e
–T
p
): (a) T 2K for > 0 (0 0.05); (b) T 10K for < 0.The small T at all optical depths given by (a) could, for example, be due to a pole-equator difference in effective temperatures. At small optical depths a difference in mechanical heating could give rise to the larger temperature difference given by (b). We compare the results of our calculations with Dicke and Goldenberg's observations.The National Center for Atmospheric Research is sponsored by the National Science Foundation. 相似文献
65.
66.
Werner?Schneider Frank?MatternEmail author PuJun?Wang Cai?Li 《International Journal of Earth Sciences》2003,92(2):228-254
The ophiolite-bearing Bangong-Nujiang zone (BNZ) traversing central Tibet from east to west separates the Qiangtang block in the north from the Lhasa block in the south. Their stratigraphic development indicates that both blocks once formed a continuous continental platform until the Late Triassic. Following Late Paleozoic-Triassic rifting, ocean crust formed between both blocks during the Late Triassic creating the Dongqiao-Naqu basin (DNB) among other basins (Yu et al. 1991). The analysis of the rift flank sequences reveals that rifting was dominated by transtension. The basin was shortened by post-Mid-Cretaceous transpression. Thus, the overall basin evolution represents a Reading cycle despite some active margin processes which gave this cycle a special imprint. Major basin parts were preserved despite transpressional shortening suggesting that the eastern BNZ represents a remnant basin. Our understanding of the DNB solves the prior problem of viewing the BNZ as a Mid-Late Jurassic collisional suture although typical collision-related deformation, thickening, mountain building, as well as related molasse formation are lacking. Our model also explains the scattered linear ophiolite distribution by local transpression of remnant oceanic basin floor without having to consider problematic long range ophiolite thrusting. 相似文献
67.
Nikolai Dotzek Peter Lang Martin Hagen Thorsten Fehr Werner Hellmiss 《Atmospheric Research》2007,83(2-4):519-533
Two downburst events from one thunderstorm are investigated, which occurred on 23 March 2001, in Germany's climatologic annual minimum of downburst activity. Observations by two Doppler radars are combined with hail reports, ground lightning detection and an aerial survey conducted after the event. The downburst-producing storm had formed at a synoptic convergence line within the warm sector of a cyclone. It had a remarkably high propagation speed of up to 31 m s− 1 corresponding to the mid-tropospheric flow. Thus, by superposition with the storm motion, even two weak downbursts were sufficient to cause the observed damage of F1 and F2 intensity, respectively. While in its late stages, the storm was dynamically characterized by lower- and mid-tropospheric divergence; at about the time of the first downburst, a mesocyclonic vortex signature was verified. Aside from mid-tropospheric dry air entrainment, a thermodynamic explanation for the triggering of the two downbursts by melting of small hail according to recent findings by Atlas et al. [Atlas, D., Ulbrich, C.W., Williams, C.R., 2004. Physical origin of a wet microburst: observations and theory. J. Atmos. Sci. 61, 1186–1196] appears probable. Despite the lack of warnings to the public, the storm's potential for hail and strong straight-line winds was detected by the German weather service radar software CONRAD more than a half hour before the downbursts occurred. 相似文献
68.
Werner Smykatz-Kloss 《Chemie der Erde / Geochemistry》2007,67(2):175-176
69.
70.
Two deterministic models were combined: one for canopy leaf energy budgets and one for street canyon energy budgets. The effects of street parks and roof gardens in contrast to non-vegetated city blocks were examined by the use of four typical urban morphologies, which were exposed latitudinally to summer and winter simulations. A variety of increases and decreases in shortwave radiation, net radiation, sensible heat flux, and system reradiation resulted. These changes appear to represent the generalized limits of the possible responses to the addition of vegetation to non-vegetated city blocks. 相似文献