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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

Alluvial record of an early Eocene hyperthermal, Castissent Formation, the Pyrenees, Spain

Autor: Honegger, L., Adatte, T., Spangenberg, J., Caves Rugenstein, J., https://orcid.org/0000-0003-4123-3305, Poyatos, M., Puigdefabregas, C., Chanvry, E., Clark, J., Fildani, A., Verrechia, E., Harlaux, M., Castelltort, S.

Publikováno v: Climate of the Past

The late Palaeocene to the middle Eocene (57.5 to 46.5 Ma) recorded a total of 39 hyperthermals – periods of rapid global warming documented by prominent negative carbon isotope excursions (CIEs) as well as peaks in iron content – have been recog

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______1874::c3e7518859bc77ec3810adfface1357f
https://hdl.handle.net/21.11116/0000-0005-A1DA-F21.11116/0000-0005-A1DC-D21.11116/0000-0005-A1DD-C

Chemical and boron isotope composition of tourmaline from the Kiaka orogenic gold deposit (Burkina Faso, West African Craton) as a proxy for ore-forming processes.

Autor: Gauriau, J., Harlaux, M., André-Mayer, A.-S., Eglinger, A., Richard, A., Fontaine, A., Lefebvre, M.G., Béziat, D., Villeneuve, J., Lemarchand, D.

Publikováno v: Mineralium Deposita; Apr2022, Vol. 57 Issue 4, p581-600, 20p

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