Thèse de doctorat en Science de la Terre
Soutenue en 2005
High-precision Pb-Pb isochron ages on inclusions (CAIs and chondrules) in meteorites will provide better understanding of the first condensation events within the solar nebula. Geochronology on differentiated meteorites and rocks of the solar system will help clarify the timing of the magmatic processes involved in the differentiation of parent bodies.
Chronology of the inner Solar System accretion and planetary differentiation
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