全文获取类型
收费全文 | 70篇 |
免费 | 2篇 |
专业分类
测绘学 | 2篇 |
大气科学 | 7篇 |
地球物理 | 8篇 |
地质学 | 37篇 |
海洋学 | 14篇 |
天文学 | 1篇 |
自然地理 | 3篇 |
出版年
2022年 | 1篇 |
2019年 | 2篇 |
2018年 | 3篇 |
2017年 | 1篇 |
2016年 | 1篇 |
2015年 | 3篇 |
2014年 | 4篇 |
2013年 | 6篇 |
2012年 | 3篇 |
2011年 | 8篇 |
2010年 | 5篇 |
2009年 | 4篇 |
2008年 | 3篇 |
2007年 | 3篇 |
2006年 | 2篇 |
2004年 | 2篇 |
2002年 | 6篇 |
2001年 | 1篇 |
2000年 | 2篇 |
1999年 | 1篇 |
1998年 | 1篇 |
1997年 | 1篇 |
1991年 | 1篇 |
1985年 | 1篇 |
1984年 | 2篇 |
1983年 | 1篇 |
1980年 | 1篇 |
1973年 | 2篇 |
1972年 | 1篇 |
排序方式: 共有72条查询结果,搜索用时 0 毫秒
71.
Hanebuth Till J. J. Kudrass Hermann R. Zander Anja M. Akhter Humayun Syed Neumann-Denzau Gertrud Zahid Anwar 《Natural Hazards》2022,111(1):163-190
Natural Hazards - This study reconstructs the coastal subsidence over the past 1300 years in a mangrove region along the coast of the Ganges–Brahmaputra Delta, an area not affected... 相似文献
72.
Evolution of the Galicia Interior Basin over the last 60 ka: sedimentary processes and palaeoceanographic implications 下载免费PDF全文
Anxo Mena Guillermo Francés Marta Pérez‐Arlucea Till J. J. Hanebuth Vera B. Bender Miguel A. Nombela 《第四纪科学杂志》2018,33(5):536-549
The Galicia Interior Basin (GIB; NW Iberian Peninsula) is located near a critical transition between the subtropical (temperate) and subpolar (cold) gyres of the North Atlantic. It therefore witnesses oceanographic changes driven by global climatic events. This study reports on the recent (latest Pleistocene) sedimentary, palaeoceanographic and palaeoclimatic history of the basin. We integrated analysis of deep‐sea sediment cores retrieved from an E–W transect across the GIB. The analysis indicated three types of sedimentary processes recording glacial (Marine Isotope Stage 2–4) and deglacial events: along‐slope bottom currents (forming contourite deposits), pelagic and hemipelagic sedimentation, and gravitational dislocation. Variation in depositional patterns and sedimentation rates indicate distinctive transport (along‐slope and down‐slope) and depositional processes. These in turn reflect climatic and oceanographic drivers. We interpret changes in sea level from core evidence showing changes in sediment supply. The cores exhibited conspicuous sedimentary evidence of Heinrich events (HEs). The stratigraphic intervals associated with HEs showed significant lateral variation. We suggest that the lateral variation may result from the development of an oceanographic boundary between surface water masses with different temperature and salinity parameters or changes in surface currents which may have introduced relatively warmer water into the GIB during the last glacial period. 相似文献