摘要
锆石SHRIMPU-Pb年龄测定表明,科克赛花岗闪长斑岩体形成年龄为(317±6)Ma.结合区域地质及物探成果分析,判定科克赛花岗闪长斑岩体形成时代为晚石炭世.据近年发现的与该岩体有关的铜钼矿产情况分析,认为该岩体具有寻找铜钼矿产的前景.
Zircon SHRIMP U-Pb dating manifest that Keersai granite diorite-porphyry body date is （317±6） Ma. The regional geology situation and the physical prospecting achievement explain the formation time of Keersai granite diorite-porphyry body belongs to Upper Carboniferous.According to the recent years discovered copper molybdenum minerals related with this rock mass, it thought this rock mass has perspective to seek the copper molybdenum minerals.
出处
《新疆地质》
CAS
CSCD
2008年第4期340-342,共3页
Xinjiang Geology
关键词
博乐市
花岗闪长斑岩
锆石
SHRIMP定年
晚石炭世
Granite diorite-porphyry
Zircon
SHRIMP U-Pb dating
Upper Carboniferous
Bole city
Xinjiang
