Petrology of the Yugu peridotites in the Gyeonggi Massif, South Korea: Implications for its origin and hydration process-Reference-Cited by-同舟云学术

Petrology of the Yugu peridotites in the Gyeonggi Massif, South Korea: Implications for its origin and hydration process

Published:2008-12 Issue:4 Volume:17 Page:485-501
ISSN:1038-4871
Container-title:Island Arc
language:en
Short-container-title:

Author:

Arai Shoji,Tamura Akihiro,Ishimaru Satoko,Kadoshima Kazuyuki,Lee Yong-Il,Hisada Ken-ichiro

Publisher

Wiley

Subject

Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1440-1738.2008.00633.x/fullpdf

Reference73 articles.

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2. Characterization of spinel peridotites by olivine-spinel compositional relationships: Review and interpretation;Arai;Chemical Geology,1994

3. Petrology of peridotite xenoliths in alkali basalt (11 Ma) from Boun, Korea: An insight into the upper mantle beneath the East Asian continental margin;Arai;Journal of Mineralogical and Petrological Sciences,2001

4. The Mid-Atlantic Ridge near 45°N. XVI. Serpentinized ultramafic intrusions;Aumento;Canadian Journal of Earth Sciences,1971

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2. Microstructural evolution of the Yugu peridotites in the Gyeonggi Massif, Korea: Implications for olivine fabric transition in mantle shear zones;Tectonophysics;2017-07

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