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   54篇
  免费   1篇
  55篇
  2020年   1篇
  2019年   2篇
  2018年   2篇
  2017年   2篇
  2016年   5篇
  2015年   6篇
  2013年   22篇
  2012年   1篇
  2011年   1篇
  2010年   2篇
  2008年   1篇
  2007年   1篇
  1997年   1篇
  1995年   1篇
  1984年   1篇
  1981年   1篇
  1980年   2篇
  1977年   1篇
  1976年   1篇
  1973年   1篇
排序方式: 共有55条查询结果,搜索用时 0 毫秒
1.
The subject of this paper is the Livre des propriétés des choses, the fourteenth-century French translation of the thirteenth-century encyclopedia De proprietatibus rerum. The translation was made for Charles V of France, and the original copy is lost. Here a reconstruction is offered of the appearance of the frontispiece of the royal exemplar. The textual additions of the translator and the iconography of this frontispiece reveal a new conception of the meaning and usage of the encyclopedia, as well as a concerted attempt to draw this authoritative work into the orbit of royal aims and aspirations. The reconstructed frontispiece also allows us to correct an error, which originates with Montfaucon, concerning the illustration of the original copy of the Livre des propriétés des choses.  相似文献   
2.
    
This paper identifies and investigates the distribution patterns, physical properties and cultural associations of the four types of rock art found on Uneapa Island, West New Britain, Papua New Guinea. It generates a series of hypotheses relating to the production and consumption of cupules, three‐dimensional, curvilinear and rectilinear rock art, and how this may have changed through time.  相似文献   
3.
4.
5.
6.
7.
8.
W edge -shaped soil structures occur in many parts of southern Canada and the northern United States. These have usually been interpreted as being ice-wedge casts. Yehle (1954), however, has expressed concern over the confusion of fossil ice wedges with features he termed soil tongues, but also referred to as soil pendants (Wright 1961) or podsolschornsteine (Johnsonn 1959). Not only are soil tongues superficially similar to ice-wedge casts, but they also occur in temperate latitudes which may have experienced periglacial conditions during the Pleistocene. Soil tongues, however, are solutional features, formed by rainwater percolating through unconsolidated calcareous deposits. They may be distinguished from ice-wedge casts and other wedge-shaped structures by: (a) the presence of pebble or other marker beds extending unbroken across the wedges; (b) the absence of bed contortions or pressure features in the materials adjacent to the wedges; (c) their conical three-dimensional shape; and (d) the lower carbonate content in the sediments of the wedges than in the surrounding materials.  相似文献   
9.
10.
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