Copper migration and enrichment in the mantle wedge: Insights from orogenic peridotites and pyroxenites
Author:
Funder
National Natural Science Foundation of China
Fundamental Research Funds for the Central Universities
National Key Research and Development Program of China
Publisher
Elsevier BV
Reference84 articles.
1. Geochemistry of Fe-rich peridotites and associated pyroxenites from Horní Bory, Bohemian Massif: insights into subduction-related melt–rock reactions;Ackerman;Chem. Geol.,2009
2. Petrogenesis and Lu–Hf dating of (ultra)mafic rocks from the kutná hora crystalline complex: Implications for the devonian evolution of the bohemian massif;Ackerman;J. Petrol.,2020
3. Highly siderophile element geochemistry of peridotites and pyroxenites from Horní Bory, Bohemian Massif: implications for HSE behaviour in subduction-related upper mantle;Ackerman;Geochim. Cosmochim. Acta,2013
4. Re–Os and Lu–Hf isotopic constraints on the formation and age of mantle pyroxenites from the Bohemian Massif;Ackerman;Lithos,2016
5. The behavior of halogens during subduction-zone processes;Barnes,2018
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