The upper Oligocene San Rafael intrusive complex (Eastern Cordillera, southeast Peru), host of the largest-known high-grade tin deposit

Autor: Harlaux M.[1, Kouzmanov K.[1], Gialli S.[1], Clark A.H.[3], Laurent O.[4, Corthay G.[1], Prado Flores E.[1], Dini A.[5], Chauvet A.[6], Ulianov A.[7], Chiaradia M.[1], Menzies A.[8], VillÓn Durand G.[9], Kalinaj M.[9], Fontboté L.[1]

Publikováno v: Lithos
Lithos, Elsevier, 2021, 400-401, pp.106409. ⟨10.1016/j.lithos.2021.106409⟩
Lithos, 2021, 400-401, pp.106409. ⟨10.1016/j.lithos.2021.106409⟩
Lithos, 400-401
Lithos, Vol. 400-401, No 106409 (2021)
Lithos (Oslo. Print) 400-401 (2021): 1–23. doi:10.1016/j.lithos.2021.106409
info:cnr-pdr/source/autori:Harlaux M.[1,2], Kouzmanov K.[1], Gialli S.[1], Clark A.H.[3], Laurent O.[4,a], Corthay G.[1], Prado Flores E.[1], Dini A.[5], Chauvet A.[6], Ulianov A.[7], Chiaradia M.[1], Menzies A.[8], VillÓn Durand G.[9], Kalinaj M.[9], Fontboté L.[1]/titolo:The upper Oligocene San Rafael intrusive complex (Eastern Cordillera, southeast Peru), host of the largest-known high-grade tin deposit/doi:10.1016%2Fj.lithos.2021.106409/rivista:Lithos (Oslo. Print)/anno:2021/pagina_da:1/pagina_a:23/intervallo_pagine:1–23/volume:400-401

The upper Oligocene San Rafael intrusive complex (SRIC), located at the southwest margin of the Eastern Cordillera of southeast Peru, is an exceptional case study to investigate the petrogenesis of a large composite granitic pluton associated with th

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2c0b22fc8bd8d91407d91aef69a5035d
https://hal.archives-ouvertes.fr/hal-03408136