地质通报2012，Vol.31Issue(5)：716-725,10.
赣南龙南地区余田群玄武岩SHRIMP锆石U-Pb年龄及其地质意义
SHRIMP zircon U-Pb age of Yutian Group basalts in Longnan area of southern Jiangxi Province and its geological significance
摘要
Abstract
The bimodal volcanic rocks of Yutian Group are located in Longnan, Baimianshi and Changpu basins along the EW-trending Sannan-Xunwu fault belt in southern Jiangxi Province. The zircon U-Pb dating yields the following results: the age of the basalt at the bottom of Yutian Group in Dongkeng basin is 194.4Ma±2.0Ma, whereas the age of the basalt at the top of Yutian Group in Changpu basin is 191.9Ma±2.2Ma. These dating results not only indicate that the age of Yutian Group belongs to the early Early Jurassic but also show that the basalt and the rhyolite have the same age, coincident with the stratigraphic sequence of the section and belonging to typical bimodal volcanic rocks. Age determinations of the bimodal volcanic rocks in Yutian Group provide the age evidence for the extension tectonic environment during the early Early Jurassic in southern Jiangxi Province. Meanwhile, the residual zircon (2571-222SMa) exists in the basalt of Changpu basin, which also supplies the collateral evidence to the existence of the late Neo-Archean to Palaeo-Proterozoic basement in southern Jiangxi.关键词
双峰式火山岩/SHRIMP锆石U-Pb年龄/早侏罗世早期/江西南部Key words
bimodal volcanic rocks/SHRIMP zircon U-Pb dating/early Early Jurassic/southern Jiangxi分类
天文与地球科学引用本文复制引用
项媛馨,巫建华..赣南龙南地区余田群玄武岩SHRIMP锆石U-Pb年龄及其地质意义[J].地质通报,2012,31(5):716-725,10.基金项目
中国核工业总公司地质项目《中国中、新生代铀成矿作用》(编号:中核计 2008-74号) （编号:中核计 2008-74号）
