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In situ LA‑ICP‑MS U-Pb titanite dating of Na-Ca metasomatism in orogenic belts: the North Pyrenean example

Sylvain Fallourd 1 Marc Poujol 2 Philippe Boulvais 2 Jean-Louis Paquette 3 Michel de Saint Blanquat 4 Philippe Remy
1 GR - Géosciences Rennes
2 Terre, Temps, Traçage
GR - Géosciences Rennes
3 LMV - Laboratoire Magmas et Volcans
4 GET - Géosciences Environnement Toulouse
Abstract : In the Pyrenees, in association with the rotation of the Iberian plate around Europe during the Mid- Cretaceous, a Na-Ca metasomatism is recognized as a complementary record of the hydrothermal activity that led to Na-metasomatism (albitization) and talc-chlorite mineralization. It affected metasedimentary rocks as well as Hercynian granites. In situ laser ablation ICP-MS U-Pb analyses of titanite grains formed in albitites during metasomatism date the Na-Ca metasomatism between 110 and 92 Ma. The temperature of the Na-Ca metasomatism is estimated to be approximately 550 °C. Both the time constraints and temperature estimates suggest that the Na-Ca metasomatism is related to the low-P high-T North Pyrenean metamorphism.
keyword : Na-Ca metasomatism Albitization Pyrenees Titanite LA-ICP-MS U-Pb dating
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https://hal-insu.archives-ouvertes.fr/insu-00965320
Contributor : Isabelle Dubigeon Connect in order to contact the contributor
Submitted on : Tuesday, March 25, 2014 - 9:49:36 AM
Last modification on : Tuesday, October 19, 2021 - 11:02:06 PM

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INSU | UNIV-RENNES1 | CNRS | LMV | OSUR | OMP | GR | PRES_CLERMONT | OMP-GET | GR-3T | UNIV-ST-ETIENNE | UNIV-RENNES | OPGC | UNIV-TLSE3 | UDL | METEO | UR1-ENV

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Sylvain Fallourd, Marc Poujol, Philippe Boulvais, Jean-Louis Paquette, Michel de Saint Blanquat, et al.. In situ LA‑ICP‑MS U-Pb titanite dating of Na-Ca metasomatism in orogenic belts: the North Pyrenean example. International Journal of Earth Sciences, Springer Verlag, 2014, 103 (3), pp.667-683. ⟨10.1007/s00531-013-0978-1⟩. ⟨insu-00965320⟩

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