Continental Thermal Blanketing Explains the Compositional Dichotomy of the Diffuse Basaltic Province Across Central‐Eastern Asia

Abstract A diffuse magmatic province covering central‐eastern Asia continent displays a compositional transition at 120–100 Ma and probably reflects melting initiation in isotopically enriched lithospheric mantle, followed by melting of the asthenosphere. However, the cause for the transition across...

Full description

Saved in:
Bibliographic Details
Main Authors: Hong‐Kun Dai, Jian‐Ping Zheng, Qing Xiong, William L. Griffin, Suzanne Y. O’Reilly
Format: Article
Language:English
Published: Wiley 2023-09-01
Series:Geophysical Research Letters
Online Access:https://doi.org/10.1029/2023GL104951
Tags: Add Tag
No Tags, Be the first to tag this record!