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Petrogenesis of high Ba–Sr plutons with high Sr/Y ratios in an intracontinental setting: evidence from Early Cretaceous Fushan monzonites, central North China Craton

Published online by Cambridge University Press:  13 June 2019

Xi-Yao Li Open the ORCID record for Xi-Yao Li [Opens in a new window] ,
San-Zhong Li Open the ORCID record for San-Zhong Li [Opens in a new window] ,
Feng Huang ,
Yong-Ming Wang ,
Sheng-Yao Yu ,
Hua-Hua Cao  and
Wei-Ming Xie
Xi-Yao Li
Affiliation:
Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, Institute for Advanced Ocean Study, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China Laboratory for Marine Geology and Environment, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
San-Zhong Li*
Affiliation:
Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, Institute for Advanced Ocean Study, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China Laboratory for Marine Geology and Environment, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
Feng Huang
Affiliation:
School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China
Yong-Ming Wang
Affiliation:
School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287-1404, USA
Sheng-Yao Yu
Affiliation:
Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, Institute for Advanced Ocean Study, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China Laboratory for Marine Geology and Environment, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
Hua-Hua Cao
Affiliation:
Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, Institute for Advanced Ocean Study, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China Laboratory for Marine Geology and Environment, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
Wei-Ming Xie
Affiliation:
Hebei Institute of Geological Survey, Shijiazhuang 050081, China
*
*Author for correspondence: San-Zhong Li, Email: Sanzhong@ouc.edu.cn
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Abstract

Geochronological, major and trace element, and Sr–Nd–Hf isotopic data are reported for the monzonitic rocks of the Fushan pluton in the Taihang Mountains, central North China Craton, in order to investigate their sources, petrogenesis and tectonic implications. Zircon U–Pb dating results reveal that the Fushan pluton was emplaced during the Early Cretaceous (∼126–124 Ma). The monzonites and quartz monzonites are mainly characterized by calc-alkaline and magnesian features and display light rare earth element (LREE) enrichment and flat heavy REE (HREE) patterns with slightly positive Eu anomalies. They have similar whole-rock initial 87Sr/86Sr ratios (0.70653–0.70819), εNd(t) values (−13.6 to −18.6) and zircon εHf(t) values (−21.8 to −17.3). The primary magma of the Fushan pluton was derived from the partial melting of a spinel-facies amphibole-bearing ancient enriched lithospheric mantle. The monzonitic rocks also have high Ba–Sr and low Y and Yb contents, with high Sr/Y and La/Yb ratios. These geochemical features of monzonitic rocks are not only inherited from the magma source but also significantly enhanced by crystal fractionation during magmatic evolution; e.g. hornblende fractionation increased the Ba–Sr concentrations and Sr/Y ratios. During the Early Cretaceous, the slab sinking and roll-back of the Palaeo-Pacific Plate could have created an ancient big mantle wedge beneath East Asia and induced a lithospheric extensional process in the central North China Craton within an intracontinental setting.

Keywords

Cretaceoushigh Ba–Sr plutonhigh Sr/YmonzoniteNorth China Cratonpetrogenesis
Type
Original Article
Information
Geological Magazine , Volume 156 , Issue 12 , December 2019 , pp. 1965 - 1981
Copyright
© Cambridge University Press 2019 

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Table S3

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Table S2

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Table S1

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Table S4

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