Magma mixing and magmatic-to-hydrothermal fluid evolution revealed by chemical and boron isotopic signatures in tourmaline from the Zhunuo–Beimulang porphyry Cu-Mo deposits
Author:
Funder
National Science Foundation
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s00126-024-01255-6.pdf
Reference94 articles.
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2. Bachmann O, Bergantz G (2008) The magma reservoirs that feed supereruptions. Elements 4(1):17–21
3. Beckett-Brown CE, McDonald AM, McClenaghan MB (2023) Trace element characteristics of tourmaline in porphyry Cu systems: development and application to discrimination. Canadian J Mineral Petrol 61(1):31–60
4. Blundy J, Mavrogenes J, Tattitch B, Sparks S, Gilmer A (2015) Generation of porphyry copper deposits by gas-brine reaction in volcanic arcs. Nat Geosci 8(3):235–240
5. Cao M, Evans NJ, Hollings P, Cooke DR, McInnes BI, Qin K, Li G (2018) Phenocryst zonation in porphyry-related rocks of the Baguio district, Philippines: evidence for magmatic and metallogenic processes. J Petrol 59(5):825–848
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