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Arc-related peridotite blocks exhumed to the Eastern Block of the North China Craton prior to 2.47 Ga

Published online by Cambridge University Press:  27 July 2021

Mingyue Gong Open the ORCID record for Mingyue Gong [Opens in a new window] ,
Wei Tian Open the ORCID record for Wei Tian [Opens in a new window] ,
Zhuang Li ,
Bin Fu  and
Chunjing Wei
Mingyue Gong
Affiliation:
MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing100871, China
Wei Tian*
Affiliation:
MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing100871, China
Zhuang Li
Affiliation:
State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing102249, China College of Geosciences, China University of Petroleum, Beijing102249, China Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun130061, China
Bin Fu
Affiliation:
Research School of Earth Sciences, The Australian National University, CanberraACT2601, Australia
Chunjing Wei
Affiliation:
MOE Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing100871, China
*
Author for correspondence: Wei Tian, Email: davidtian@pku.edu.cn
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Abstract

The Songling and Majiayu peridotite blocks occur in the Eastern Block, North China Craton (NCC). Geothermobarometry data show that the Songling peridotites began exhumation from a depth of c. 70 km (c. 23 kbar). During exhumation, the Songling peridotites were intruded by an upper-crust-derived, high-δ18O (up to +7.28‰ in zircon) trondhjemitic dyke at 2.47 Ga and experienced granulite-facies metamorphism. The Songling peridotites have hybrid mantle wedge (HMW) -like high SiO2 (> 45 wt%), high FeOt (c. 10 wt%) content, high modal orthopyroxene abundance (> 35%) and high ϵNd(t) (+18.4 to +21.4), which were generated by the reaction between peridotite and eclogite-derived melts. The clinopyroxenes from the Songling peridotites were in equilibrium with a Nb-, Zr- and Ti-depleted arc-like magma. The Majiayu peridotites are characterized by depletion of Nb, Zr and Hf and are highly enriched in FeOt, Th and light rare earth elements (LREEs), which can be interpreted as an open system reaction between hydrous melts and fore-arc mantle peridotites. These two peridotite blocks are considered to be arc-related mantle peridotites that experienced melt extraction and metasomatism in different styles. They were exhumed to the north margin of the North China Craton during the c. 2.47 Ga arc–continent collision along the Zunhua structural belt.

Keywords

Neoarcheanperidotitetrondhjemitic dykeNorth China Cratonexhumationarc–continent collision
Type
Original Article
Information
Geological Magazine , Volume 158 , Issue 12 , December 2021 , pp. 2115 - 2138
Copyright
© The Author(s), 2021. Published by Cambridge University Press

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