摘要
研究区分布于二连—贺根山蛇绿混杂岩带上。本次研究通过与区域泥鳅河组对比,发现古生物化石鉴定为早-中泥盆世,并在该组中取得的流纹岩锆石U-Pb同位素年龄为360±2Ma。该组的确定对西伯利亚板块和华北板块碰撞开始的时间有促进作用。
The research cloudyrespectively erlian - hegenshan back-arc ophiolitic melange belt.This study compared with regional loach river group, found fossils identified as early - middle devonian, and in the group of the rhyolite zircon U - Pb isotopic age is 360 + 2 ma.The determination of the group of the starting time of the Siberian plate and north China plates.
出处
《世界有色金属》
2017年第1期101-101,103,共2页
World Nonferrous Metals
关键词
苏尼特左旗
泥盆
大民山组
腕足类和珊瑚类化石
时代
层序特征
Sunit Zoy
Devonian
Daminshan formation
Brachiopoda and coral fossils
time sequence characteristics