 | | Journal (article/letter/editorial) | | la Houssinière - BP 92208 44322 NANTES CEDEX 3 - France CE 2 : Bureau de recherches géologiques et minières...DAT/OMR/GUY/CAY, B.P. 10552, 97333 Cayenne Cedex 2 - France *: Corresponding author (jean-pierre.lorand@univ-nantes...outcrops in south Brittany (Audierne near Quimper, Champtoceaux near Nantes), western France, were studied...crop out in the Armorican massif IP T (western France) especially in the southern part of the massif...(near Nantes) and Audierne (80 km south of Brest, Finistère) nappe-stacking complexes. We performed a multiscale |  | | Book (edition) | | 59:41–68 References Tang Y, Li X, Xie Y, Liu L, Lan T, Meffre S, Huang C (2017) Geochronology and geochemistry...2017) suggest that the breakdown of magnetite and antigorite during subduction of serpentinized oceanic crust...inherit halogens, H2O and sulfur released during antigorite breakdown (Kendrick et al. 2011, 2018; Brandt...B-rich fluids in subduction zones: the role of antigorite dehydration in subducting slabs and boron isotope...Southern-Central Variscan Vosges Mountains (NE France). J Geol Soc London 172:87–102 Taetz S, John T |  | | Book | | alteration of ultramafic rocks. Serpentine minerals (antigorite, chrysotile and lizardite) are formed from olivine...<1008C for lizardite, to as high as 5008C for antigorite. Commonly, pseudomorphs of serpentine after olivine...Dahlkamp (1993) is Limousin in the Massif Central (France), which are one of the most important sources of...Chung SL, Chua MF, Zhang YQ, Xie YG, Lo CH, Lee TY, Lan CY, Li XH, Zhang Q, Wang YZ (2005) Tibetan tectonic...125:275–315 Pierret MC, Clauer N, Bosch D, Blanc G, France-Lanord C (2001) Chemical and isotopic (87Sr/86Sr |
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