Evolution of the magmatic-hydrothermal system at the Erdenetiin Ovoo porphyry Cu-Mo deposit, Mongolia: constraints on the relative timing of alteration and mineralization-Reference-Cited by-同舟云学术

Evolution of the magmatic-hydrothermal system at the Erdenetiin Ovoo porphyry Cu-Mo deposit, Mongolia: constraints on the relative timing of alteration and mineralization

Published:2023-12-19 Issue: Volume: Page:
ISSN:0026-4598
Container-title:Mineralium Deposita
language:en
Short-container-title:Miner Deposita

Author:

Monecke Thomas^ORCID,Reynolds T. James,Gonchig Tsolmon,Batbayar Natsagdorj

Funder

Erdenet Mining Corporation

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Link

https://link.springer.com/content/pdf/10.1007/s00126-023-01221-8.pdf

Reference100 articles.

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3. Arancibia ON, Clark AH (1996) Early magnetite-amphibole-plagioclase alteration-mineralization in the Island Copper porphyry copper-gold-molybdenum deposit, British Columbia. Econ Geol 91:402–438

4. Arif J, Baker T (2004) Gold paragenesis and chemistry at Batu Hijau, Indonesia: implications for gold-rich porphyry copper deposits. Miner Depos 39:523–535

5. Audétat A (2023) A plea for more skepticism toward fluid inclusions: Part II. Homogenization via halite dissolution in brine inclusions from magmatic-hydrothermal systems is commonly the result of postentrapment modifications. Econ Geol 118:43–55

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