Post-collisional alkaline magmatism as gateway for metal and sulfur enrichment of the continental lower crust-Reference-Cited by-同舟云学术

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Post-collisional alkaline magmatism as gateway for metal and sulfur enrichment of the continental lower crust

Published:2018-02 Issue: Volume:223 Page:175-197
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Fiorentini Marco L.,LaFlamme Crystal,Denyszyn Steven,Mole David,Maas Roland,Locmelis Marek,Caruso Stefano,Bui Thi-Hao

Funder

ARC Centre of Excellence for Core to Crust Fluid Systems

Australian Research Council

Future Fellowship Scheme

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference88 articles.

1. The capacity of hydrous fluids to transport and fractionate incompatible elements and metals within the Earth’s mantle;Adam;Geochem. Geophys. Geosyst.,2014

2. On the processes that formed Archaean Ni-Cu sulfide mineralisation in the deep continental crust, Thrym Complex, southeastern Greenland;Bagas;Precambr. Res.,2016

3. TEMORA 1: a new zircon standard for Phanerozoic U-Pb geochronology;Black;Chem. Geol.,2003

4. The mineral system approach applied to magmatic Ni–Cu–PGE sulphide deposits;Barnes;Ore Geol. Rev.,2016

5. Lithospheric, cratonic, and geodynamic setting of Ni–Cu–PGE sulfide deposits;Begg;Econ. Geol.,2010

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4. Archean atmospheric sulfur stocked in the Cretaceous gold deposits;Geochemistry;2024-06

5. Incipient carbonate melting drives metal and sulfur mobilization in the mantle;Science Advances;2024-03-22

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