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Bruno Goffé

Researcher at Aix-Marseille University

Publications -  142
Citations -  12529

Bruno Goffé is an academic researcher from Aix-Marseille University. The author has contributed to research in topics: Metamorphism & Nappe. The author has an hindex of 62, co-authored 142 publications receiving 11383 citations. Previous affiliations of Bruno Goffé include Centre national de la recherche scientifique & Schlumberger.

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Raman spectra of carbonaceous material in metasediments: a new geothermometer

Olivier Beyssac, +3 more
- 01 Dec 2002 - 
TL;DR: In this article, the degree of organisation of carbonaceous material was systematically characterised by Raman microspectroscopy across several Mesozoic and Cenozoic reference metamorphic belts.
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On the characterization of disordered and heterogeneous carbonaceous materials by Raman spectroscopy.

Olivier Beyssac, +5 more
- 01 Aug 2003 - 
TL;DR: A new Raman technique (Raman area mode microspectroscopy) giving an homogeneous repartition of power within a large laser beam is presented, this technique being powerful to study strongly heterogeneous CM and/or photosensitive samples.
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Midcrustal shear zones in postorogenic extension: Example from the northern Tyrrhenian Sea

Laurent Jolivet, +10 more
- 10 Jun 1998 - 
TL;DR: In this article, a model for ductile extension and metamorphic evolution in the northern Tyrrhenian Sea from Alpine Corsica to Tuscany is presented. But the model involves retreat of the slab and migration of the volcanic arc.
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Subduction tectonics and exhumation of high pressure metamorphic rocks in the Mediterranean orogens

Laurent Jolivet, +4 more
- 01 May 2003 - 
TL;DR: In this article, the authors discuss the mechanisms of syn-orogenic exhumation of high pressure (HP) and ultra-high pressure (UHP) rocks in the peri-Mediterranean blueschist belts.
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Evolution of the Raman spectrum of carbonaceous material in low‐grade metasediments of the Glarus Alps (Switzerland)

Abdeltif Lahfid, +6 more
- 01 Oct 2010 - 
TL;DR: The Raman spectrum of carbonaceous material (CM) from advanced diagenesis to low-grade metamorphism (∼320°C) is documented in the Helvetic flysch of the Glarus Alps (Switzerland) as mentioned in this paper.