Petrologic origin of exsolution textures in mantle minerals: evidence in pyroxenitic xenoliths from Yakutia kimberlites-Reference-Cited by-同舟云学术

Petrologic origin of exsolution textures in mantle minerals: evidence in pyroxenitic xenoliths from Yakutia kimberlites

Published:2011-11-30 Issue:9 Volume:54 Page:1071-1092
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Alifirova Taisia Aleksandrovna¹,Pokhilenko Lyudmila Nikolaevna¹,Ovchinnikov Yuriy Ivanovich¹,Donnelly Cara Lyhn²,Riches Amy J.V.²,Taylor Lawrence August²

Affiliation:

1. a V.S. Sobolev Institute of Geology and Mineralogy , Siberian Branch, Russian Academy of Science , Novosibirsk , Russia , 630090

2. b Department of Earth and Planetary Sciences , Planetary Geosciences Institute, University of Tennessee , Knoxville , TN , 37996 , USA

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2011.623011

Reference118 articles.

1. Afanas'ev, V.P., Zinchuk, N.N. and Pokhilenko, N.P. 2001.Morphology and morphogenesis of indicator minerals in kimberlites, 276Novosibirsk, Izdatel'stvo, SO RAN: Filial “Geo”. in Russian

2. Rb-Sr and Sm-Nd isotopes in garnet pyroxenite xenoliths from Siberian kimberlites: an insight into lithospheric mantle.

3. Exsolved garnet-bearing pyroxene megacrysts from some South African kimberlites

4. Two mantle sources, two plumbing systems: tholeiitic and alkaline magmatism of the Maymecha River basin, Siberian flood volcanic province

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