The gold content of mafic to felsic potassic magmas.

Autor: Chang J; Bavarian Geoinstitute, University of Bayreuth, Bayreuth, 95440, Germany. Jia.Chang@uni-bayreuth.de., Audétat A; Bavarian Geoinstitute, University of Bayreuth, Bayreuth, 95440, Germany., Pettke T; Institute of Geological Sciences, University of Bern, Bern, 3012, Switzerland.

Publikováno v: Nature communications [Nat Commun] 2024 Aug 14; Vol. 15 (1), pp. 6988. Date of Electronic Publication: 2024 Aug 14.

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Magmatic genesis, hydration, and subduction of the tholeiitic eclogite-facies Allalin gabbro (Western Alps, Switzerland).

Autor: Dietrich J; Institute of Geological Sciences, University of Bern, Baltzerstrasse 1+3, 3012 Bern, Switzerland., Hermann J; Institute of Geological Sciences, University of Bern, Baltzerstrasse 1+3, 3012 Bern, Switzerland., Pettke T; Institute of Geological Sciences, University of Bern, Baltzerstrasse 1+3, 3012 Bern, Switzerland.

Publikováno v: Swiss journal of geosciences [Swiss J Geosci] 2024; Vol. 117 (1), pp. 12. Date of Electronic Publication: 2024 Jun 19.

Fingerprinting and relocating tectonic slices along the plate interface: Evidence from the Lago Superiore unit at Monviso (Western Alps)

Autor: Gilio M.[1, Scambelluri M.[1], Agostini S.[3], Godard M.[4], Pettke T.[5], Agard P.[6], Locatelli M.[6], Angiboust S.[7]

Publikováno v: Lithos
Lithos, Elsevier, 2020, 352-353, pp.105308. ⟨10.1016/j.lithos.2019.105308⟩
Lithos (Oslo. Print) 352-353 (2020). doi:10.1016/j.lithos.2019.105308
info:cnr-pdr/source/autori:Gilio M.[1,2], Scambelluri M.[1], Agostini S.[3], Godard M.[4], Pettke T.[5], Agard P.[6], Locatelli M.[6], Angiboust S.[7]/titolo:Fingerprinting and relocating tectonic slices along the plate interface: Evidence from the Lago Superiore unit at Monviso (Western Alps)/doi:10.1016%2Fj.lithos.2019.105308/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:352-353

International audience; The Lago Superiore Unit (LSU, Monviso Massif, Italian Western Alps) is a section of fossil oceanic lithosphere equilibrated to eclogite facies conditions (550 °C – 2.8 GPa) during Alpine subduction (45–40 Ma). It is cut b

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a43c5b9bcda29c70fbe58e10967a3c8f
https://hal.umontpellier.fr/hal-02510337

Petrology and geochemistry of serpentinites associated with the ultra-high pressure Lago di Cignana unit (Italian Western Alps)

Autor: Gilio M.[1, Scambelluri M.[1, Agostini S.[3], Godard M.[4], Peters D.[5, Pettke T.[5]

Publikováno v: Journal of petrology
60 (2019): 1229–1262. doi:10.1093/petrology/egz030
info:cnr-pdr/source/autori:Gilio M.[1,2], Scambelluri M.[1,3], Agostini S.[3], Godard M.[4], Peters D.[5,6], Pettke T.[5]/titolo:Petrology and geochemistry of serpentinites associated with the ultra-high pressure Lago di Cignana unit (Italian Western Alps)/doi:10.1093%2Fpetrology%2Fegz030/rivista:Journal of petrology (Print)/anno:2019/pagina_da:1229/pagina_a:1262/intervallo_pagine:1229–1262/volume:60
Gilio, M.; Scambelluri, M.; Agostini, S.; Godard, M.; Peters, Daniel; Pettke, Thomas (2019). Petrology and Geochemistry of Serpentinites Associated with the Ultra-High Pressure Lago di Cignana Unit (ItalianWestern Alps). Journal of petrology, 60(6), pp. 1229-1262. Oxford University Press 10.1093/petrology/egz030

In the Western Alps, the ophiolitic Zermatt–Saas Zone (ZSZ) and the Lago di Cignana Unit (LCU) record oceanic lithosphere subduction to high (540°C, 2·3GPa) and ultra-high pressure (600°C, 3·2GPa), respectively. The top of the Zermatt–Saas Zo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::613242a4b73a4d722be13c6faf498b37
https://publications.cnr.it/doc/465143