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Late Jurassic, high Ba–Sr Linglong granites in the Jiaodong Peninsula, East China: lower crustal melting products in the eastern North China Craton

Published online by Cambridge University Press:  26 January 2017

LI-QIANG YANG ,
YILDIRIM DILEK ,
ZHONG-LIANG WANG ,
ROBERTO F. WEINBERG  and
YUE LIU
LI-QIANG YANG*
Affiliation:
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
YILDIRIM DILEK
Affiliation:
Department of Geology & Environmental Earth Science, Miami University, Oxford, OH 45056, USA
ZHONG-LIANG WANG
Affiliation:
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
ROBERTO F. WEINBERG
Affiliation:
School of Earth, Atmosphere & Environment, Monash University, Victoria 3800, Australia
YUE LIU
Affiliation:
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China School of Earth Sciences, The University of Melbourne, Victoria 3010, Australia
*
†Author for correspondence: lqyang@cugb.edu.cn
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Abstract

The Jurassic Linglong granites, intrusive into the North China Craton (NCC) in eastern China, provide a critical record of the first major episode of lithospheric-scale extension and magmatism in NE China during Mesozoic time. Our U–Pb zircon dating reveals that the Linglong granites were emplaced during 161–158 Ma, shortly after the inception of a shallow subduction of the Palaeo-Pacific plate beneath East Asia during Middle Jurassic time. These granites have high alkali contents (K2O + Na2O = 8–9 wt%), low MgO and Mg no. values and variable Cr–Ni abundances. Their relatively high Ba and Sr concentrations, relatively low heavy rare Earth element (HREE) and strongly fractionated REE patterns characterize them as high Ba–Sr granites. The negative whole-rock εNd(t) values ranging from −22.4 to −10.9 and wide-ranging zircon εHf(t) values of −39.1 to −1.5 suggest that magmas of the Linglong granites were produced by partial melting of a garnet-amphibolite-bearing lower crust of the Jiaobei Terrane and by re-melting of the Triassic ultrahigh-pressure (UHP) metamorphic rocks and alkaline suites of the Sulu Terrane. The occurrence in the granitic rocks of inherited zircons of the Neoarchaean, Palaeoproterozoic, Neoproterozoic, Palaeozoic and Triassic ages suggests that magmas of the Linglong granites interacted with the ancient crust in these terranes during their ascent. Asthenospheric upwelling, induced by the steepening and rapid rollback of the Palaeo-Pacific slab during Late Jurassic time, provided the heat source for the inferred lower crustal melting. Trench migration and thermal weakening of the crust caused extensional deformation and thinning in the eastern part of the NCC.

Keywords

high Ba–Sr granitesLate Jurassic magmatismNorth China Cratongranitic magmatism
Type
Original Article
Information
Geological Magazine , Volume 155 , Issue 5 , July 2018 , pp. 1040 - 1062
Copyright
Copyright © Cambridge University Press 2017 

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