Mg and Si isotopic fractionation patterns in types B1 and B2 CAIs: Implications for formation under different nebular conditions-Reference-Cited by-同舟云学术

Mg and Si isotopic fractionation patterns in types B1 and B2 CAIs: Implications for formation under different nebular conditions

Published:2013-07-30 Issue:8 Volume:48 Page:1440-1458
ISSN:1086-9379
Container-title:Meteoritics & Planetary Science
language:en
Short-container-title:Meteorit Planet Sci

Author:

Bullock Emma S.¹,Knight Kim B.²,Richter Frank M.³,Kita Noriko T.⁴,Ushikubo Takayuki⁴,MacPherson Glenn J.¹,Davis Andrew M.,Mendybaev Ruslan A.³

Affiliation:

1. US National Museum of Natural History; Smithsonian Institution; Washington; District of Columbia; 20560; USA

2. Lawrence Livermore National Laboratory; 7000 East Avenue; Livermore; California; 94550-9234; USA

3. Department of the Geophysical Sciences; University of Chicago; Chicago; 60637; USA

4. Department of Geosciences; University of Wisconsin-Madison; Madison; Wisconsin; 53706; USA

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/maps.12158/fullpdf

Reference34 articles.

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2. The partitioning of Na between melilite and liquid: Part I. The role of crystal chemistry and liquid composition;Beckett;Geochimica et Cosmochimica Acta,2000

3. Forsterite-bearing type B refractory inclusions from CV3 chondrites: From aggregates to volatilized melt droplets;Bullock;Meteoritics & Planetary Science,2012

4. Isotopic variations in the rock-forming elements in meteorites;Clayton;Philosophical Transactions of the Royal Society of London,1988

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