全文获取类型
收费全文 | 72篇 |
免费 | 2篇 |
国内免费 | 8篇 |
专业分类
测绘学 | 10篇 |
大气科学 | 7篇 |
地球物理 | 4篇 |
地质学 | 26篇 |
海洋学 | 24篇 |
综合类 | 5篇 |
自然地理 | 6篇 |
出版年
2023年 | 1篇 |
2021年 | 2篇 |
2020年 | 1篇 |
2015年 | 1篇 |
2014年 | 6篇 |
2013年 | 6篇 |
2012年 | 2篇 |
2011年 | 2篇 |
2010年 | 7篇 |
2009年 | 4篇 |
2008年 | 15篇 |
2007年 | 4篇 |
2006年 | 3篇 |
2005年 | 2篇 |
2004年 | 6篇 |
2003年 | 2篇 |
2002年 | 1篇 |
2001年 | 1篇 |
1999年 | 1篇 |
1998年 | 1篇 |
1997年 | 3篇 |
1996年 | 2篇 |
1995年 | 3篇 |
1992年 | 1篇 |
1991年 | 2篇 |
1990年 | 2篇 |
1937年 | 1篇 |
排序方式: 共有82条查询结果,搜索用时 187 毫秒
2.
3.
4.
5.
Variations of δ18O in the snow which accumulates at a Nordic temperate glacier during the win-ter are not entirely eliminated after a few months of ablation in the following summer. Survive of isotopicsignals closely relates to the re-freezing capacity of snow accumulated in winter when its temperature wasbelow 0 ℃. The melt-water re-freezing ice layers formed in winter hindered subsequent melt-water percolation in summer when snow temperature was at melting point and, therefore, varied isotopic record wasreserved between these ice layers. The isotopic record in snow pack can provide an estimate of the ap-proximate trend of the most recent winter season temperatures. The relationship between regional tem-perature changes and δ18O values in the snow pack is affected by many natural factors, but 1989-1990 (aglacier balance year) winter air temperatures were reflected in the snow which remained on the glacierAustre Okstindbreen at an altitude of 1 350 m in July 1990. There was larger amplitude of variations ofδ18O values in the 4. 1 m of snow above the 1989 summer surface, but variations in the underlying firnwere relatively small. Melt water percolation modifies the initial variations of δ18O values in the snowpack. At a site below the mean equilibrium line altitude on Austre Okstindbreen, increased isotopic bom-ogenization within a ten-day period in July accompanied an increase of the mean δ18O value. Although theisotopic record at a temperate glacier is likely to be influenced by more factors than is that at polar glac-iers, it can provide an estimate of the approximate trend of recent local temperature variations. 相似文献
6.
7.
北极大陆架面积约2600×10^4km2,这片广阔的大陆架地区被分为若干盆地和潜在油气区。俄罗斯北极区内有两大地块,即东部地块和西部地块。这两大地块均形成于陆壳基底之上,被Gakkel扩张脊和邻近的深水拗陷隔歼,并于晚元古代、泥盆纪、晚二叠世-二叠纪和白垩纪-早第三纪的裂陷作用阶段被多次改造。西部地块由巴伦支海一喀拉海陆架组成,且延伸至两拉普帖夫海;东部地块则由拉普贴夫海东部、东西伯利亚和Chukcha盆地所组成。 相似文献
8.
Jan Inge Faleide Filippos Tsikalas AsbjФrn Breivik Rolf Mjelde Oliver Ritzmann Фyvind Engen Jonas Wilson Olav Eldholm 《《幕》》2008,31(1):82-91
The Norwegian Margin formed in response to early Cenozoic continental breakup and subsequent opening of the Norwegian-Greenland Sea. There is a welldefined margin segmentation and the various segments are characterized by distinct crustal properties, structural and magmatic styles, and post-opening history of vertical motions. The sedimentary basins at the conjugate continental margins off Norway and Greenland and in the western Barents Sea developed as a result of a series of post-Caledonian rift episodes until early Cenozoic time, when complete continental separation took place. 相似文献
9.
挪威斯塔万格大学科技学院前院长佩尔·阿内尔·比约库姆和挪威国家石油公司两位研究员经过10年研究,最近提出了油气勘探黄金地带理论,并经过了全球12万个已知油气田数据的验证。 相似文献
10.
The Proterozoic Bamble Sector, South Norway, is one of the world's classic amphiboliteto granulite- facies transition zones. It is characterized by a well-developed isograd sequence, with isolated 'granulite-facies islands' in the amphibolite-facies portion of the transition zone. The area is notable for the discovery of C02-dominated fluid inclusions in the granolite-facies rocks by Jacques Touter in the late 1960's, which triggered discussion of the role of carbonic fluids during granulite genesis. The aim of this review is to provide an overview of the current state of knowledge of the Bamble Sector, with an emphasis on the Arendal-Froland-Nelaug-Tvedestrand area and off shore islands (most prominantly Tromay and Hisoy) where the transition zone is best developed. After a brief overview of the history of geological research and mining in the area, aspects of sedimentary, metamorphic and magmatic petrology of the Bamble Sector are discussed, including the role of fluids. Issues relevant to current geotectonic models for SW Scandinavia, directly related to the Bamble Sector, are discussed at the end of the review. 相似文献