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Constraints of magmatism on the Ergu Fe–Zn polymetallic metallogenic system in the central Lesser Xing’an Range, NE China: evidence from geochronology, geochemistry and Sr–Nd–Pb–Hf isotopes

Published online by Cambridge University Press:  23 July 2021

Chuntao Zhao ,
Jinggui Sun Open the ORCID record for Jinggui Sun [Opens in a new window] ,
Yang Liu ,
Xiaolei Chu ,
Zhikai Xu ,
Jilong Han ,
Wenqing Li ,
Liang Ren  and
Chenglin Bai
Chuntao Zhao
Affiliation:
College of Earth Science, Jilin University, Changchun130061, China Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun130061, China
Jinggui Sun*
Affiliation:
College of Earth Science, Jilin University, Changchun130061, China Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun130061, China
Yang Liu
Affiliation:
College of Earth Science, Jilin University, Changchun130061, China
Xiaolei Chu
Affiliation:
College of Earth Science, Jilin University, Changchun130061, China
Zhikai Xu
Affiliation:
College of Earth Science, Jilin University, Changchun130061, China
Jilong Han
Affiliation:
School of Earth Sciences and Resources, China University of Geosciences, Beijing100083, China
Wenqing Li
Affiliation:
Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun130061, China
Liang Ren
Affiliation:
College of Earth Science, Jilin University, Changchun130061, China
Chenglin Bai
Affiliation:
College of Earth Science, Jilin University, Changchun130061, China
*
Author for correspondence: Jinggui Sun, Email: [email protected]
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Abstract

The medium-sized Ergu Fe–Zn polymetallic skarn deposit is located in the central Lesser Xing’an Range, NE China. The ore bodies are mainly hosted in the contact zone between granodiorite intrusions and lower Cambrian dolomitic crystalline limestones or skarns. To reveal the magmatic influence on the mineralization, resource potential and metallogenic geodynamic process of this deposit, a systematic study of the geology, petrology, zircon U–Pb dating, element geochemistry, amphibole geochemistry and Sr–Nd–Pb–Hf isotopes of the Ergu deposit intrusives was conducted. The results show the following: (1) The major rock types in the mine area are medium-grained granodiorite and porphyritic granite, and the rock related to mineralization is medium-grained granodiorite. Zircon U–Pb dating suggests that the granodiorite and porphyritic granite formed at 181.9–183.8 Ma and 182.7 Ma, respectively. Thus, an Early Jurassic magmatic event led to the formation of the Ergu deposit. (2) The granodiorite and porphyritic granite are high-K calc-alkaline I-type granites that formed by comagmatic evolution with varying degrees of fractional crystallization and were likely derived from partial melting of the lower crust. The Ergu deposit occurred in an active continental-margin tectonic setting. (3) The high water content (5.69 wt % H2O), high oxygen fugacity (ΔFMQ = +1.75 to +1.82) and intermediate-plutonic emplacement (3.13 km) of the granodioritic magma are key factors in the formation of the Ergu deposit. The porphyry granite is characterized by high water content (>4 wt % H2O), reduced oxygen fugacity (ΔFMQ = −0.47) and shallow emplacement (<3 km).

Keywords

element geochemistrySr–Nd–Pb–Hf isotope geochemistryzircon U–Pb datingintermediate-plutonic magmatismErgu depositLesser Xing’an Range
Type
Original Article
Information
Geological Magazine , Volume 158 , Issue 10 , October 2021 , pp. 1862 - 1890
Copyright
© The Author(s), 2021. Published by Cambridge University Press

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