Polymetamorphic P–T evolution of the andalusite–garnet–staurolite–sillimanite-bearing schist from the Cushamen Complex (Argentina)
Author:
Funder
Fondo para la Investigación Científica y Tecnológica
Universidad Nacional de Córdoba
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s00531-024-02437-3.pdf
Reference89 articles.
1. Ague J, Axler J (2016) Interface coupled dissolution-reprecipitation in garnet from subducted granulites and ultrahigh-pressure rocks revealed by phosphorous, sodium, and titanium zonation. Am Miner 101(7):1696–1699. https://doi.org/10.2138/am-2016-5707
2. Baxter EF, Caddick MJ, Ague JJ (2013) Garnet: common mineral, uncommonly useful. Elements 9(6):415–419. https://doi.org/10.2113/gselements.9.6.415
3. Baxter EF, Caddick MJ, Dragovic B (2017) Garnet: a rock-forming mineral petrochronometer. Rev Miner Geochem 83(1):469–533. https://doi.org/10.2138/rmg.2017.83.15
4. Bovay T, Lanari P, Rubatto D, Smit M, Piccoli F (2021) Pressure–temperature–time evolution of subducted crust revealed by complex garnet zoning (Theodul Glacier Unit, Switzerland). J Metamorph Geol 40:175–206. https://doi.org/10.1111/jmg.12623
5. Caddick MJ, Konopásek J, Thompson AB (2010) Preservation of garnet growth zoning and the duration of prograde metamorphism. J Petrol 51(11):2327–2347. https://doi.org/10.1093/petrology/egq059
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