THE EARLY-CRETACEOUS TECTONIC EVOLUTION AND THE SPATIAL-TEMPORAL FRAMEWORK OF MAGMATISM-MINERALIZATION IN ZIJINSHAN ORE-FIELD, FUJIAN PROVINCE

PAN Tianwang; YUAN Yuan; LYU Yong; SHI Wenqiang

doi:10.12090/j.issn.1006-6616.2019.25.01.007

Volume 25 Issue 1

Feb. 2019

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PAN Tianwang, YUAN Yuan, LYU Yong, et al., 2019. THE EARLY-CRETACEOUS TECTONIC EVOLUTION AND THE SPATIAL-TEMPORAL FRAMEWORK OF MAGMATISM-MINERALIZATION IN ZIJINSHAN ORE-FIELD, FUJIAN PROVINCE. Journal of Geomechanics, 25 (1): 61-76. DOI: 10.12090/j.issn.1006-6616.2019.25.01.007

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THE EARLY-CRETACEOUS TECTONIC EVOLUTION AND THE SPATIAL-TEMPORAL FRAMEWORK OF MAGMATISM-MINERALIZATION IN ZIJINSHAN ORE-FIELD, FUJIAN PROVINCE

doi: 10.12090/j.issn.1006-6616.2019.25.01.007

PAN Tianwang^{1, 2
,},
YUAN Yuan^{3
,
,},
LYU Yong^{1, 2},
SHI Wenqiang^{1, 2}

1.
Institute of Karst Geology, CAGS, Guilin 541004, Guangxi, China
2.
Key Laboratory of Karst Dynamics, MNR & GZAR, Guilin 541004, Guangxi, China
3.
School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China

More Information

Received: 2017-10-10
Revised: 2018-05-22
Published: 2019-02-01

Abstract

Abstract

This paper presents a systematic review of major types and characteristics of the representative deposits in the Zijinshan ore-field by integrating with previous studies, which is in an attempt to establish the spatial-temporal framework of magmatic-metallogenic events during 145~92 Ma time interval and, on that basis, investigate its relationship with the NW-trending Shanghang-Yunxiao mineralization belt under the Early Cretaceous extension setting. We conclude that the magmatism-mineraliztion of the Zijinshan ore-field was mainly controlled by the multiple activation of the NW-trending Shanghang-Yunxiao deep fault in response to Pacific plate subduction. There occurred a small scale of the magmatism and metallogenesis in the Zijinshan ore-field when the regional tectonic regime inversed from compression to extension (145~125 Ma), whereas the intense crust-mantle interaction induced large scale of magmatism and mineralization during the 110~92 Ma in response to the enhanced crust extension, which resulted in generating the giant Zijinshan porphyry-epithermal Cu-Au-Mo-Ag ore system. It's worth noting that a transient tectonic inversion lasted from 125~110 Ma separated the two extension stage mentioned above. These transpression gave rise to the short magmatic quiescence in our study area.

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THE EARLY-CRETACEOUS TECTONIC EVOLUTION AND THE SPATIAL-TEMPORAL FRAMEWORK OF MAGMATISM-MINERALIZATION IN ZIJINSHAN ORE-FIELD, FUJIAN PROVINCE

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THE EARLY-CRETACEOUS TECTONIC EVOLUTION AND THE SPATIAL-TEMPORAL FRAMEWORK OF MAGMATISM-MINERALIZATION IN ZIJINSHAN ORE-FIELD, FUJIAN PROVINCE

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