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Petrogenesis of Early Cretaceous adakites from the Liaodong Peninsula: insight into the lithospheric thinning of the North China Craton

Published online by Cambridge University Press:  28 July 2022

Chao Wang
Affiliation:
College of Earth Sciences, Jilin University, No. 2199 Jianshe Street, Changchun 130061, China Jilin Institute of Geological Survey, Changchun 130061, China
Jinlei Sun
Affiliation:
College of Earth Sciences, Jilin University, No. 2199 Jianshe Street, Changchun 130061, China State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
Yanjie Shen*
Affiliation:
College of Earth Sciences, Jilin University, No. 2199 Jianshe Street, Changchun 130061, China Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Nature Resources of China, No. 2199 Jianshe Street, Changchun 130061, China
Tao Tian
Affiliation:
The Fifth Geological Exploration Institute of Qinghai Province, No. 42 Chaoyang West Street, Xining 810000, China
Jinyu Li
Affiliation:
College of Earth Sciences, Jilin University, No. 2199 Jianshe Street, Changchun 130061, China State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
Ye Qian
Affiliation:
College of Earth Sciences, Jilin University, No. 2199 Jianshe Street, Changchun 130061, China Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Nature Resources of China, No. 2199 Jianshe Street, Changchun 130061, China
Fengyue Sun
Affiliation:
College of Earth Sciences, Jilin University, No. 2199 Jianshe Street, Changchun 130061, China Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Nature Resources of China, No. 2199 Jianshe Street, Changchun 130061, China
*
Author for correspondence: Yanjie Shen, Email: shenyjjlu@sina.com

Abstract

Lithospheric thinning occurred in the North China Craton (NCC) that resulted in extensive Mesozoic magmatism, which has provided the opportunity to explore the mechanism of the destruction of the NCC. In this study, new zircon U–Pb ages, geochemical and Lu–Hf isotopic data are presented for Early Cretaceous adakitic rocks in the Liaodong Peninsula, with the aim of establishing their origin as well as the thinning mechanism of the NCC. The zircon U–Pb data show that crystallization occurred during 127–120 Ma (i.e. Early Cretaceous). These rocks are characterized by high Sr (294–711 ppm) content and Sr/Y ratio (38.5–108), low Yb (0.54–1.24 ppm) and Y (4.9–16.4 ppm) contents, and with no obvious Eu anomalies, implying that they are adakitic rocks. They are enriched in large-ion lithophile elements (e.g. Ba, K, Pb and Sr) and depleted in high-field-strength elements (e.g. Nb, Ta, P and Ti). These adakitic rocks have negative zircon ϵ Hf(t) contents (−28.9 to −15.0) with two-stage Hf model ages (T DM2) of 3004–2131 Ma. Based on the geochemical features, such as low TiO2 and MgO contents, and high La/Yb and K2O/Na2O ratios, these adakites originated from the partial melting of thickened eclogitic lower crust. They were in an extensional setting associated with the slab rollback of the Palaeo-Pacific Ocean. In combination with previous studies, as a result of the rapid retracting of the Palaeo-Pacific Ocean during 130–120 Ma, the asthenosphere upwelled and modified the thickened lithospheric mantle, which lost its stability, resulting in the lithospheric delamination and thinning of the NCC.

Type
Original Article
Copyright
© The Author(s), 2022. Published by Cambridge University Press

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