Comment on "Ultra-high pressure and ultra-reduced minerals in ophiolites may form by lightning strikes"

W. L. Griffin; D. Howell; J. M. Gonzalez-Jimenez; Q. Xiong; S. Y. O'Reilly

doi:10.7185/geochemlet.1809

Comment on "Ultra-high pressure and ultra-reduced minerals in ophiolites may form by lightning strikes"

W. L. Griffin, D. Howell, J. M. Gonzalez-Jimenez, Q. Xiong, S. Y. O'Reilly

ARC Centre of Excellence for Core to Crust Fluid Systems (incorporation ARC National Key Centre for Geochemical evolution and Metallogeny of Continents (GEMOC))

Research output: Contribution to journal › Comment/opinion › peer-review

15 Citations (Scopus)

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Original language	English
Pages (from-to)	1-2
Number of pages	2
Journal	Geochemical Perspectives Letters
Volume	7
DOIs	https://doi.org/10.7185/geochemlet.1809
Publication status	Published - 1 Jan 2018

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Copyright the Author(s) 2018. Version archived for private and non-commercial use with the permission of the author/s and according to publisher conditions. For further rights please contact the publisher.

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10.7185/geochemlet.1809

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AU - Xiong, Q.

AU - O'Reilly, S. Y.

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Comment on "Ultra-high pressure and ultra-reduced minerals in ophiolites may form by lightning strikes"

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