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Lithospheric thinning of the North China craton: Insights from Early Cretaceous intermediate–mafic dyke swarms in Jiaodong peninsula.

Authors :
Ji, Lei
Liu, Junlai
Ding, Xu
Luo, Zhiming
Ni, Jinlong
Shi, Xiaoxiao
Nam Dao, Hai
Source :
Gondwana Research; Jul2022, Vol. 107, p84-106, 23p
Publication Year :
2022

Abstract

[Display omitted] • Intermediate–mafic dyke swarms in Jiaodong peninsula are dated (122–121 Ma). • The dykes were formed in a WNW-ESE oriented extensional stress field. • Tectono-magmatic processes at crust–mantle depths were decoupled along the Moho. • Destruction of the lithospheric keel in southeastern NCC occurred at 122–120 Ma. • Tectonic extension acted as the major driving force for destruction of the craton. The coupling/decoupling relationships between shallow crustal deformation and deep mantle tectono-magmatic activities, during lithospheric thinning and destruction of cratons, remain hotly debated in the last decades. Multidisciplinary studies were done on intermediate–mafic dyke swarms diffusively located in southern Jiaodong peninsula, southeastern North China craton (NCC) to explore the crustal and lithospheric mantle responses to regional tectonic extension. Uniform ages (122–121 Ma) of the dykes indicate intensive magma generation at the mantle depth around 122 Ma related to large-scale tectonic extension of regional lithospheric mantle. Systemic anisotropy of magnetic susceptibility (AMS), geochemical, and Sr-Nd isotope analyses suggest that the dykes were originated from enriched lithospheric mantle sources and emplaced along crustal fractures formed in a WNW-ESE oriented extensional stress field. We show that the Jiaodong lithosphere experienced two stages of Early Cretaceous tectonic evolution, i.e., an early stage (135–122 Ma) lithospheric thinning characterized by large-scale tectonic extension of the crust and limited magmatic activities of crustal sources, and a late stage (122–108 Ma) lithospheric root collapse dominated by intensive tectonic extension and magmatism in the lithospheric mantle level. The decoupling crust-mantle evolution during lithospheric thinning and destruction of the NCC is ascribed to continuous tectonic extension in WNW-ESE direction. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
1342937X
Volume :
107
Database :
Supplemental Index
Journal :
Gondwana Research
Publication Type :
Academic Journal
Accession number :
156894433
Full Text :
https://doi.org/10.1016/j.gr.2022.01.020