全文获取类型
| 收费全文 | 42篇 |
| 免费 | 0篇 |
专业分类
| 地球物理 | 9篇 |
| 地质学 | 6篇 |
| 海洋学 | 23篇 |
| 天文学 | 1篇 |
| 自然地理 | 3篇 |
出版年
| 2016年 | 1篇 |
| 2013年 | 2篇 |
| 2010年 | 1篇 |
| 2008年 | 1篇 |
| 2006年 | 2篇 |
| 2005年 | 1篇 |
| 2004年 | 2篇 |
| 2003年 | 2篇 |
| 2002年 | 1篇 |
| 2000年 | 1篇 |
| 1997年 | 2篇 |
| 1994年 | 1篇 |
| 1992年 | 1篇 |
| 1986年 | 1篇 |
| 1984年 | 3篇 |
| 1982年 | 1篇 |
| 1980年 | 3篇 |
| 1979年 | 2篇 |
| 1978年 | 1篇 |
| 1977年 | 1篇 |
| 1976年 | 2篇 |
| 1975年 | 1篇 |
| 1973年 | 1篇 |
| 1971年 | 1篇 |
| 1969年 | 1篇 |
| 1968年 | 4篇 |
| 1966年 | 2篇 |
排序方式： 共有42条查询结果，搜索用时 31 毫秒
1.
2.
The decline of the herring stocks and the gadoid outburst 总被引：2，自引：1，他引：2
3.
4.
5.
6.
The gadoid outburst in the North Sea 总被引：3，自引：3，他引：3
7.
John Cushing Marla Daily Elmer Noble V. Louise Roth Adrian Wenner 《Quaternary Research》1984,21(3):376-384
Mammoth remains on Santa Cruz Island, one of the four Northern Channel Islands of California, are very sparse, in marked contrast to those reported from Santa Rosa and San Miguel Islands of the same island group. A probable major reason for this scarcity is that Quaternary deposits are greatly restricted on Santa Cruz Island. It is proposed, contrary to popular opinion, that fossils found on Santa Cruz Island were derived from animals which died on the island, and were not transported there by humans. Reasons for this conclusion are that the size and geological context of the fossils are similar to those of the largest mammoth fossils of Santa Rosa Island, and that, in spite of extensive investigations by many persons, mammoth remains have not been found in middens, either on the islands or on the adjacent mainland. 相似文献
8.
E. M. Cushing O. Bellier S. Nechtschein M. Sébrier A. Lomax Ph. Volant P. Dervin P. Guignard L. Bove 《Geophysical Journal International》2008,172(3):1163-1178
Assessing seismic hazard in continental interiors is difficult because these regions are characterized by low strain rates and may be struck by infrequent destructive earthquakes. In this paper, we provide an example showing that interpretations of seismic cross sections combined with other kinds of studies such as analysis of microseismicity allow the whole seismogenic source area to be imaged in this type of region. The Middle Durance Fault (MDF) is an 80-km-long fault system located southeastern France that has a moderate but regular seismicity and some palaeoseismic evidence for larger events. It behaves as an oblique ramp with a left-lateral-reverse fault slip and has a low strain rate. MDF is one of the rare slow active fault system monitored by a dedicated dense velocimetric short period network. This study showed a fault system segmented in map and cross section views which consists of staircase basement faults topped by listric faults ramping off Triassic evaporitic beds. Seismic sections allowed the construction of a 3-D structural model used for accurate location of microseismicity. Southern part of MDF is mainly active in the sedimentary cover. In its northern part and in Alpine foreland, seismicity deeper than 8 km was also recorded meaning active faults within the crust cannot be excluded. Seismogenic potential of MDF was roughly assessed. Resulting source sizes and estimated slip rates imply that the magnitude upper limit ranges from 6.0 to 6.5 with a return period of a few thousand years. The present study shows that the coupling between 3-D fault geometry imaging and accurate location of microseismicity provides a robust approach to analyse active fault sources and consequently a more refined seismic hazard assessment. 相似文献
9.
10.