Identification of the EMII-type mantle end-member of the Kerguelen mantle plume and its implications for the initial breakup of eastern Gondwana: New constraints from the Cretaceous diabase in the Tethyan Himalaya-Reference-Cited by-同舟云学术

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Identification of the EMII-type mantle end-member of the Kerguelen mantle plume and its implications for the initial breakup of eastern Gondwana: New constraints from the Cretaceous diabase in the Tethyan Himalaya

Published:2024-08 Issue: Volume:272 Page:106250
ISSN:1367-9120
Container-title:Journal of Asian Earth Sciences
language:en
Short-container-title:Journal of Asian Earth Sciences

Author:

Meng Fanxue,Meng Yuanku^ORCID,Wei Youqing

Publisher

Elsevier BV

Reference142 articles.

1. The geochemical regimes of Piton de la Fournaise volcano (Reunion) during the last 530,000 years;Albarède;J. Petrol.,1997

2. Petrogenetic evolution of late Cenozoic, post-collision volcanism in western Anatolia, Turkey;Aldanmaza;J. Volcanol. Geoth. Res.,2000

3. Pb isotopic analysis of standards and samples using a 207Pb–204Pb double spike and thallium to correct for mass bias with a double-focusing MC-ICP-MS;Baker;Chem. Geol.,2004

4. Paleomagnetic and geochronological results from the Zhela and Weimei formations lava flows of the eastern Tethyan Himalaya: new insights into the breakup of eastern Gondwana;Bian;J. Geophys. Res. Solid Earth,2019

5. Petrology and geochemistry of Camiguin Island, southern Philippines: insights to the source of adakites and other lavas in a complex arc setting;Castillo;Contrib. Miner. Petrol.,1999

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