Titanium isotopes and rare earth patterns in CAIs: Evidence for thermal processing and gas-dust decoupling in the protoplanetary disk-Reference-Cited by-同舟云学术

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Titanium isotopes and rare earth patterns in CAIs: Evidence for thermal processing and gas-dust decoupling in the protoplanetary disk

Published:2018-01 Issue: Volume:221 Page:275-295
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Davis Andrew M.,Zhang Junjun,Greber Nicolas D.,Hu Jingya,Tissot François L.H.,Dauphas Nicolas

Funder

U.S. National Aeronautics and Space Administration

U.S. National Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference87 articles.

1. The galactic evolution of Si, Ti, and O isotopic ratios;Alexander;Astrophys. J.,1999

2. Fractionation in the solar nebula: condensation of yttrium and the rare earth elements;Boynton;Geochim. Cosmochim. Acta,1975

3. Mg and Si isotopic fractionation patterns in types B1 and B2 CAIs: implications for formation under different nebular conditions;Bullock;Meteorit. Planet. Sci.,2013

4. Evidence for Mo isotope fractionation in the solar nebula and during planetary differentiation;Burkhardt;Earth Planet. Sci. Lett.,2014

5. Presolar corundum and spinel in ordinary chondrites: origins from AGB Stars and a supernova;Choi;Science,1998

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