Crustal melting above a mantle plume: Insights from the Permian Tarim Large Igneous Province, NW China

Low Nb-Ta rhyolites from the Permian Tarim Large Igneous Province (LIP) represent the melting products of continental crust above a mantle plume. Zircon U-Pb dating reveals that the Kuchehe and Dawanqi rhyolites were erupted at 292.6 +/- 0.5 Ma and 274 +/- 2 Ma respectively. Both rhyolite groups are...

Full description

Bibliographic Details
Published in:Lithos
Main Authors: Liu, Hai-Quan, Xu, Yi-Gang, Zhong, Yu-Ting, Luo, Zhen-Yu, Mundil, Roland, Riley, Teal R., Zhang, Le, Xie, Wei
Format: Report
Language:English
Published: ELSEVIER SCIENCE BV 2019
Subjects:
Geochemistry & Geophysics
Mineralogy
ZIRCON U-PB
LARGE-VOLUME
ANTARCTIC PENINSULA
HIGH-TEMPERATURE
LITHOSPHERE INTERACTION
RHYOLITIC VOLCANISM
YELLOWSTONE HOTSPOT
CALDERA COMPLEXES
SILICIC VOLCANISM
ISOTOPIC EVIDENCE
Antarctic
Antarctic Peninsula
Patagonia
Antarc*
Online Access:http://ir.gig.ac.cn/handle/344008/52653
https://doi.org/10.1016/j.lithos.2018.12.031
Description
Summary:Low Nb-Ta rhyolites from the Permian Tarim Large Igneous Province (LIP) represent the melting products of continental crust above a mantle plume. Zircon U-Pb dating reveals that the Kuchehe and Dawanqi rhyolites were erupted at 292.6 +/- 0.5 Ma and 274 +/- 2 Ma respectively. Both rhyolite groups are characterized by pronounced negative Nb-Ta anomalies, crust-like trace element ratios and negative epsilon(Nd-Hf)(t) values, consistent with a crustal origin. Newly acquired data, combined with available data in the literature, clearly show that there is an increasing trend of zircon saturation temperature (T-Zr) from 794 to 827 degrees C to 886-936 degrees C for the early to middle stage (293-287 Ma), followed by a decreasing T-Zr of 803-908 degrees C for the late stage (287-274 Ma) of the Tarim magmatism. The temporal changes in T-Zr for the Tarim rhyolites are interpreted to reflect the crustal melting behavior above a mantle plume, such that fusible materials in the crust melt at an earlier stage and refractory materials melt at a later stage. The gradual decrease in T-Zr, towards the final stage of the Tarim rhyolitic magmatism, reflects the gradual 'decay' of thermal input from mantle plume to the lithosphere in the region. This thermal model is also applicable to describe the crustal melting behavior in the Chon Aike silicic LIP of Patagonia and the Snake River Plateau-Yellowstone Plateau volcanic provinces. (C) 2018 Elsevier B.V. All rights reserved.

Similar Items