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Title: New minerals in type A inclusions from Allende and clues to processes in the early solar system: Paqueite, Ca 3 TiSi 2 (Al,Ti,Si) 3 O 14 , and burnettite, CaVAlSiO 6
Abstract

Paqueite (Ca3TiSi2[Al,Ti,Si]3O14; IMA 2013‐053) and burnettite (CaVAlSiO6; IMA 2013‐054) are new refractory minerals, occurring as euhedral to subhedral crystals within aluminous melilite in A‐WP1, a type A Ca‐Al‐rich inclusion, andCGft‐12, a compact type A (CTA) from the Allende CV3 carbonaceous chondrite. Type paqueite from A‐WP1 has an empirical formula of (Ca2.91Na0.11)Ti4+Si2(Al1.64Ti4+0.90Si0.24V3+0.12Sc0.07Mg0.03)O14, with a trigonal structure in space groupP321 and cell parametersa = 7.943 Å,c = 4.930 Å, V = 269.37 Å3, andZ = 1. Paqueite’s general formula is Ca3TiSi2(Al,Ti,Si)3O14and the endmember formula is Ca3TiSi2(Al2Ti)O14. Type burnettite fromCGft‐12has an empirical formula of Ca1.01(V3+0.56Al0.25Mg0.18)(Si1.19Al0.81)O6. It assumes a diopside‐typeC2/cstructure witha = 9.80 Å,b = 8.85 Å,c = 5.36 Å, β = 105.6°,V = 447.7 Å3, andZ = 4. Burnettite’s general formula is Ca(V,Al,Mg)AlSiO6and the endmember formula is CaVAlSiO6. Paqueite and burnettite likely originated as condensates, but the observed grains may have crystallized from local V‐rich melts produced during a later thermal event. ForCGft‐12, the compositions of paqueite, clinopyroxene, and perovskite suggest that type As drew from two distinct populations of grains. Hibonite grains drew from multiple populations, but these were well mixed and not equilibrated prior to incorporation into type A host melilite.

 
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NSF-PAR ID:
10445959
Author(s) / Creator(s):
 ;  ;  ;  
Publisher / Repository:
Wiley-Blackwell
Date Published:
Journal Name:
Meteoritics & Planetary Science
Volume:
57
Issue:
6
ISSN:
1086-9379
Page Range / eLocation ID:
p. 1300-1324
Format(s):
Medium: X
Sponsoring Org:
National Science Foundation
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