Two mineralization events in the Baiyinnuoer Zn-Pb deposit in Inner Mongolia, China: evidence from field observations, S-Pb isotopic compositions and U-Pb zircon ages
作者: Si-Hong JiangChun-Liang ChenLeon BagasYuan LiuNing HanHuan KangZe-Hai Wang
作者单位: 1MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, CAGS, Beijing 100037, China
2School of Earth Sciences and Resources, China University of Geosciences, Beijing 526020, China
3Centre for Exploration Targeting, The University of Western Australia, Crawley, WA 6009, Australia
4Inner Mongolia Chifeng Institute of Geology and Mineral Exploration and Development, Chifeng, Inner Mongolia 024005, China)
刊名: Journal of Asian Earth Sciences, 2016
来源数据库: Elsevier Journal
DOI: 10.1016/j.jseaes.2016.12.042
关键词: mineralization eventsuperimpositionS-Pb isotopesBaiyinnuoer Pb-Zn depositInner Mongolia
英文摘要: Abstract(#br)The Xing–Mong Orogenic Belt (XMOB) is located in the eastern part of the Central Asian Orogenic Belt (CAOB) and has experienced multiple tectonic events. The Baiyinnuoer Pb-Zn deposit may be a rare case that documents two periods of mineralization in the tectonically complex XMOB. There are two types of Pb-Zn mineralization in the deposit: (1) skarn-type ore, hosted by the skarn in the contact zone between marble and granodiorite and within the marble and (2) vein-type ore, hosted by crystal tuff and feldspar porphyry. This study revealed that the host rocks, mineral assemblages, mineralization occurrences, S-Pb isotopes, and ages between the two types of ore are notably different. Zircon U-Pb dating indicates that the granodiorite was emplaced in the Early Triassic (244 ± 1...
全文获取路径: Elsevier  (合作)
影响因子:2.379 (2012)

  • zircon 锆石
  • isotopic 同位素置换
  • deposit 沉积
  • mineralization 成矿酌
  • China 中国
  • events 定时
  • field 
  • evidence