Maxence Regnault
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View article: Origin of the volatile element depletion in carbonaceous chondrites: Insights from Zn and Cu isotope compositions of chondrules
Origin of the volatile element depletion in carbonaceous chondrites: Insights from Zn and Cu isotope compositions of chondrules Open
Introduction:Carbonaceous chondrites (CCs) are among the most primitive rock samples in our solar system. All CC groups are depleted in volatile elements (i.e., elements having 50% condensation temperature lower than ~1300 K) relative to C…
View article: Spinel in CV chondrules: Investigating precursor legacy and chondrule thermal histories
Spinel in CV chondrules: Investigating precursor legacy and chondrule thermal histories Open
In carbonaceous chondrites, Mg‐spinel (MgAl 2 O 4 ) grains are ubiquitous in refractory inclusions but rarely reported in chondrules, where they may correspond to minerals either (i) inherited from chondrule precursors or (ii) crystallized…
View article: Oxygen isotope systematics of chondrules in Rumuruti chondrites: Formation conditions and genetic link with ordinary chondrites
Oxygen isotope systematics of chondrules in Rumuruti chondrites: Formation conditions and genetic link with ordinary chondrites Open
Rumurutiites (R chondrites) are rare, highly oxidized chondrites belonging to the noncarbonaceous superclan and characterized by low chondrule abundances. Although textural and chemical features of Rumurutiite chondrules resemble those of …