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皖东苏家湾地区三里陈岩体LA-ICP-MS锆石U-Pb年代学研究
引用本文:雷丁尔,张赞赞,蔡晓兵,夏立元,王松.皖东苏家湾地区三里陈岩体LA-ICP-MS锆石U-Pb年代学研究[J].沉积与特提斯地质,2019,39(4):79-89.
作者姓名:雷丁尔  张赞赞  蔡晓兵  夏立元  王松
作者单位:1. 安徽省地质调查院(安徽省地质科学研究所), 安徽 合肥 230001;2. 合肥工业大学图书馆, 安徽 合肥 230001
基金项目:中国地质调查局南京地质调查中心项目《安徽滁县-江苏盱眙找矿远景区1:5万地质矿产综合调查》(编号:[2016]041-D32)
摘    要:三里陈岩体位于长江中下游成矿带滁县-庐江铜金成矿亚带中部,岩性主要为闪长岩和花岗闪长斑岩,LA-ICP-MS锆石U-Pb定年测得闪长岩年龄为126.9±1.8Ma,花岗闪长斑岩锆石U-Pb年龄为126.0±1.0Ma,两者均为早白垩世岩浆活动的产物。闪长岩中存在的大量继承锆石的年龄分布在2.5~1.9Ga之间,峰值为2.0Ga,暗示其岩浆源区主要为华南板块,可能混有华北板块源区的物质。结合滁县-庐江铜金成矿亚带成岩时代及矿化特征,发现三里陈岩体与铜金矿床(点)成矿岩体的形成时代相近,岩性一致,与围岩接触带发育的蚀变和矿化特征相似,认为这些侵入岩体均为同一构造-岩浆-成矿事件的产物,三里陈岩体及其外围地区具有寻找一定规模矽卡岩型铜金矿床的潜力。

关 键 词:闪长岩  LA-ICP-MS锆石U-Pb定年  皖东苏家湾地区  三里陈岩体
收稿时间:2019/8/7 0:00:00
修稿时间:2019/9/9 0:00:00

LA-ICP-MS zircon U-Pb age dating of the Sanlichen intrusion in the Sujiawan region, eastern Anhui
LEI Dinger,ZHANG Zanzan,CAI Xiaobing,XIA Liyuan,WANG Song.LA-ICP-MS zircon U-Pb age dating of the Sanlichen intrusion in the Sujiawan region, eastern Anhui[J].Sedimentary Geology and Tethyan Geology,2019,39(4):79-89.
Authors:LEI Dinger  ZHANG Zanzan  CAI Xiaobing  XIA Liyuan  WANG Song
Institution:1. Anhui Institute of Geological Survey, Hefei 230001, Anhui, China;2. Library, Hefei University of Technology, Hefei 230001, Anhui, China
Abstract:The Sanlichen intrusion is located in the central part of the Chuxian-Lujiang copper-gold metallogenic subzone in the Middle-Lower Yangtze River Valley metallogenic zone, where diorite and granodiorite are accentuated. The present paper presents two groups of high-resolution zircon U-Pb ages:126.9±1.8 Ma for the diorite and 126.0±1.0 Ma for the granodiorite. Both the diorites and granodiorites are originated from the Early Cretaceous magmatic activity. The inherited zircon U-Pb ages mainly range from 2.5 to 1.9 Ga, and the peak age is about 2.0 Ga. These data show that the magmas may be derived from the South China plate, with the mixtures of the North China plate. The similarities in mineralization age and lithology between the Sanlichen intrusion and the copper-gold deposits, and those in alteration and mineralization between the Sanlichen intrusion and the country rocks show that the intrusive rocks should be the products of the same tectonic-magmatic-mineralization events. The Sanlichen intrusion and its surrounding areas are believed to be prospective for the exploration of the skarn-type copper-gold deposits.
Keywords:diorite  LA-ICP-MS zircon U-Pb age dating  Sujiawan region in eastern Anhui  Sanlichen intrusion
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