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Sébastien Jégo

Researcher at Centre national de la recherche scientifique

Publications -  10
Citations -  229

Sébastien Jégo is an academic researcher from Centre national de la recherche scientifique. The author has contributed to research in topics: Adakite & Mafic. The author has an hindex of 7, co-authored 10 publications receiving 201 citations. Previous affiliations of Sébastien Jégo include University of Orléans.

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Metasomatic interactions between slab-derived melts and depleted mantle: Insights from xenoliths within Monglo adakite (Luzon arc, Philippines)

TL;DR: In this article, an undeformed clinopyroxene characterized by convex-upwards REE pattern was found in the mantle section of an Early Cretaceous supra-subduction zone ophiolitic complex located within the Luzon arc crust.
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Controls on Gold Solubility in Arc Magmas: An Experimental Study at 1000°C and 4 kbar

TL;DR: In this paper, the solubility of gold at 4 kbar and 1000°C for three intermediate magmas (two adakites and one calc-alkaline composition) from the Philippines were determined.
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Geochemistry of Adakites from the Philippines: Constraints on Their Origins

TL;DR: The authors identified in the Philippine Archipelago 230 samples of Late Miocene to Quaternary intermediate and evolved magmatic rocks or glasses, the compositions of which plot within the adakitic field defined by Defant and Drummond (1990) using Sr/Y ratios versus Y contents.
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Temporal geochemical evolution of Neogene magmatism in the Baguio gold-copper mining district (Northern Luzon, Philippines)

TL;DR: Baguio, in the Central Cordillera of Northern Luzon, is a district that displays porphyry copper and epithermal gold mineralization, associated with Early Miocene - Pliocene - Quaternary calc-alkaline and adakitic intrusions.
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The oceanic substratum of Northern Luzon: Evidence from xenoliths within Monglo adakite (the Philippines)

TL;DR: A suite of ultramafic and mafic xenoliths including spinel dunites showing typical mantle-related textures, mineral and bulk rock compositions, and serpentinites derived from them, amphibole-rich gabbros displaying incompatible element patterns similar to those of flat or moderately enriched back-arc basin basalt magmas, and amphibolite derived from metabasalts and/or metagabbros of identical affinity has been sampled.