首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   101篇
  免费   2篇
大气科学   8篇
地球物理   24篇
地质学   27篇
海洋学   21篇
天文学   12篇
自然地理   11篇
  2023年   1篇
  2020年   1篇
  2018年   1篇
  2017年   1篇
  2016年   2篇
  2015年   3篇
  2014年   6篇
  2013年   12篇
  2012年   2篇
  2011年   1篇
  2010年   3篇
  2009年   6篇
  2008年   8篇
  2007年   4篇
  2006年   5篇
  2005年   5篇
  2004年   3篇
  2003年   1篇
  2002年   3篇
  2001年   2篇
  2000年   6篇
  1999年   1篇
  1998年   1篇
  1997年   2篇
  1996年   2篇
  1995年   2篇
  1993年   2篇
  1990年   2篇
  1989年   1篇
  1987年   1篇
  1986年   2篇
  1985年   4篇
  1984年   2篇
  1983年   2篇
  1981年   1篇
  1979年   2篇
排序方式: 共有103条查询结果,搜索用时 15 毫秒
101.
The routes and timing of human occupation of the Tibetan Plateau (TP) are crucial for understanding the evolution of Tibetan populations and associated paleoclimatic conditions. Many archeological sites have been found in/around the Tarim Basin, on the northern margin of the Tibetan Plateau. Unfortunately, most of these sites are surface sites and cannot be directly dated. Their ages can only be estimated based on imprecise artifact comparisons. We recently found and dated an archeological site on a terrace along the Keriya River. Our ages indicate that the site was occupied at ~ 7.0–7.6 ka, making it the earliest well-dated archeological site yet identified in the Tarim Basin. This suggests that early human foragers migrated into this region prior to ~ 7.0–7.6 ka during the early to mid-Holocene climatic optimum, which may have provided the impetus for populating the region. We hypothesize that the Keriya River, together with the other rivers originating from the TP, may have served as access routes onto the TP for early human foragers. These rivers may also have served as stepping stones for migration further west into the now hyper-arid regions of the Tarim Basin, leading ultimately to the development of the Silk Road.  相似文献   
102.
103.
The use of latest Pleistocene-Holocene paleosols in defining Chinese climatic sequences is plagued by poor chronological controls caused primarily by the use of radiocarbon dates derived from bulk soil carbon. Dating of a post-glacial aeolian/paleosol sequence in the Pigeon Mountain basin of north-central China, using culturally deposited charcoal, support a wide array of other data suggesting the Younger Dryas was a period of cooler dryer conditions marked by wide-spread aeolian deposition. Periods of soil formation and higher lake levels bracket this climatic event. Climatic variability immediately before, during and immediately after the Younger Dryas interval is associated with rapid technological elaboration and innovation in the production and use of chipped stone tools, and perhaps, ground stone. © 1998 John Wiley & Sons, Inc.  相似文献   
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号