Low Mo mobility during the laterization of ultramafic bedrock: Evidence from the East Sulawesi Ophiolite, Indonesia-Reference-Cited by-同舟云学术

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Low Mo mobility during the laterization of ultramafic bedrock: Evidence from the East Sulawesi Ophiolite, Indonesia

Published:2024-08 Issue: Volume:660 Page:122150
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Damanik Adrianus,Wille Martin,Ahmad Qasid,Chatterjee Sukalpa,Crowe Sean A.,Bauer Kohen W.,Grosjean Martin,Cahyarini Sri Yudawati,Bijaksana Satria,Russell James M.,Vogel Hendrik

Funder

National Science Foundation

Deutsche Forschungsgemeinschaft

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung

Publisher

Elsevier BV

Reference75 articles.

1. The Molybdenum isotope subduction recycling conundrum: a case study from the Tongan subduction zone, Western Alps and Alpine Corsica;Ahmad;Chem. Geol.,2021

2. Molybdenum isotopes in plume-influenced MORBs reveal recycling of ancient anoxic sediments;Ahmad;Geochemical Perspectives Letters,2022

3. Heavy Mo isotope enrichment in the Pitcairn plume: Implications for the subduction cycle of anoxic sediments;Ahmad;Earth Planet. Sci. Lett.,2023

4. Identification of three dominant rainfall regions within Indonesia and their relationship to sea surface temperature;Aldrian;Int. J. Climatol.,2003

5. The isotopic signature of the global riverine molybdenum flux and anoxia in the ancient oceans;Archer;Nat. Geosci.,2008

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