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Provenance and depositional history of the Mesozoic Sanjiang Basin (northeastern China): implications for the uplift history of the northeastern Asian continental margin

Published online by Cambridge University Press:  03 November 2021

Jin-Peng Luan Open the ORCID record for Jin-Peng Luan [Opens in a new window] ,
Gideon Rosenbaum Open the ORCID record for Gideon Rosenbaum [Opens in a new window]  and
Jian-Fei Fu
Jin-Peng Luan
Affiliation:
Key Laboratory of Ministry of Education for Safe Mining of Deep Metal Mines, Northeastern University, Shenyang 110819, China School of Earth and Environmental Sciences, University of Queensland, Brisbane 4072, Queensland, Australia
Gideon Rosenbaum
Affiliation:
School of Earth and Environmental Sciences, University of Queensland, Brisbane 4072, Queensland, Australia
Jian-Fei Fu*
Affiliation:
Key Laboratory of Ministry of Education for Safe Mining of Deep Metal Mines, Northeastern University, Shenyang 110819, China
*
Author for correspondence: Jian-Fei Fu, Email: [email protected]
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Abstract

The uplift history of northeastern Asian continental margin has been the subject of much debate. The Sanjiang Basin is an ideal area to investigate the uplift history of this margin. We present new data from sandstone petrology, whole-rock geochemistry, U–Pb geochronology and Hf isotopy of detrital zircons to trace the provenance of the basin and to unravel the uplift history of the northeastern Asian continental margin. We investigated the chemical and plagioclase indices of alteration and index of compositional variability (CIA, PIA and ICV, respectively) in samples from two formations. The geochemical proxies indicate that source rocks were subjected to an intensified weathering process. Based on the high SiO2/Al2O3 values and low K2O, we infer that the two basinal strata experienced silicification and insignificant potassium metasomatism. Sandstone petrography is indicative of low degrees of sedimentary sorting, suggesting a proximal deposition. The provenance fingerprints of light rare earth, high-field-strength and transition metal elements indicate that parts of the provenance included recycled sediments, and that first-cycle sediments were derived mainly from felsic rocks with a minor contribution from intermediate and mafic rocks. The combined detrital zircon U–Pb ages and Hf isotopic results constrain the contributions of different source terranes over time. The provenance results, in combination with seismic profile interpretations from the Sanjiang Basin, suggest that the northeastern Asian continental margin experienced at least three stages of uplift, which were driven by subduction initiation of the Paleo-Pacific Ocean during the Jurassic Period, a plate motion change during the Early Cretaceous Epoch, and a shallowing of the slab dip angle during the Late Cretaceous Epoch.

Keywords

Sanjiang Basinprovenanceuplift historydetrital zircongeochemical proxies
Type
Original Article
Information
Geological Magazine , Volume 159 , Issue 3 , March 2022 , pp. 389 - 406
Copyright
© The Author(s), 2021. Published by Cambridge University Press

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