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Laurent Jolivet

Researcher at Pierre-and-Marie-Curie University

Publications -  7
Citations -  1076

Laurent Jolivet is an academic researcher from Pierre-and-Marie-Curie University. The author has contributed to research in topics: Blueschist & Crust. The author has an hindex of 7, co-authored 7 publications receiving 1023 citations. Previous affiliations of Laurent Jolivet include École Normale Supérieure.

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Exhumation of the Schistes Lustrés complex: in situ laser probe 40Ar/39Ar constraints and implications for the Western Alps

TL;DR: In this article, the Schistes Lustres (SL) suture zone occupies a key position in the Alpine chain between the high pressure Brianconnais domain and the ultra high pressure (UHP) Dora Maira massif, and reached subduction depths ranging from c. 40-65 km (Cottian Alps).
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Exhumation of Syros and Sifnos metamorphic rocks (Cyclades, Greece). New constraints on the P-T paths

TL;DR: In this paper, a multi-equilibrium approach involving several end members and solid-solution models for chlorite, phengite, and garnet is used to estimate the stability P-T conditions of different parageneses.
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Relation between the intensity of deformation and retrogression in blueschist metapelites of Tinos Island (Greece) evidenced by chlorite mica local equilibria

TL;DR: In this article, the compositional variability of chlorite and K-white mica in metapelites sampled along a NE-SW cross-section is characteristic of their P-T conditions of crystallization and is mainly characterized by variations of their Si, Al, Fe and Mg contents due to the Tschermak substitution.
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Tectonometamorphic evolution of the Schistes Lustres Complex; implications for the exhumation of HP and UHP rocks in the Western Alps

TL;DR: In this paper, structural and metamorphic data on the Schistes Lustres complex is presented, showing that conditions increase progressively from west to east from ca. 12-13 kbar/300-350 degrees C to 20-21kbar/450-500 degrees C close to the Dora Maira massif.
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Subduction, convergence and the mode of backarc extension in the Mediterranean region

TL;DR: In this paper, the authors show that the sense of shear along crustal-scale detachments is toward the trench when subduction proceeds with little or no convergence and away from the trench in the case of true convergence (Aegean).