摘要
本文通过对塔里木盆地西南部早白垩世风成沙丘的前积层产状的测量,恢复了当时的古风向和古风带。研究结果表明:当时盛行东北风,研究区属于东北信风带,正好位于北半球中低纬度沙漠带之中。
The dips of the foreset beds of the Early Cretaceous eolian dunes in southwestern Tarim Basin, Xinjiang are measured and the palaeowind directions and palaeowind belts are reconstructed in this study. The results of research show that the northeast winds were prevailing and the northeast trade wind belts predominated during the Early Cretaceous. It follows that the study area was just located in the low and middle latitude desert zones of the Northern Hemisphere during the Early Cretaceous.
出处
《沉积与特提斯地质》
CAS
CSCD
2009年第4期1-4,共4页
Sedimentary Geology and Tethyan Geology
基金
国家自然科学基金(批准号:40372064)
关键词
塔里木盆地
早白垩世
风成沙丘
古风向
古风带
Tarim Basin
Early Cretaceous
eolian dune
palaeowind direction
palaeowind belt