Paleoproterozoic SEDEX-type stratiform mineralization overprinted by Mesozoic vein-type mineralization in the Qingchengzi Pb-Zn deposit, Northeastern China

Volume: 184, Pages: 104009 - 104009
Published: Oct 1, 2019
Abstract
The Qingchengzi Pb–Zn deposit is located in the northeastern Jiao–Liao–Ji Belt (JLJB), North China Craton (NCC). Field observation and age dating indicate that the deposit was formed from Paleoproterozoic sedimentary exhalative (SEDEX) stratiform mineralization overprinted by Late Triassic hydrothermal vein-type mineralization. Five types of fluid inclusions (FIs) are identified in the quartz grains, based on petrography and laser Raman...
Paper Details
Title
Paleoproterozoic SEDEX-type stratiform mineralization overprinted by Mesozoic vein-type mineralization in the Qingchengzi Pb-Zn deposit, Northeastern China
Published Date
Oct 1, 2019
Volume
184
Pages
104009 - 104009
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