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Comment 2 on “Ultra-high pressure and ultra-reduced minerals in ophiolites may form by lightning strikes”

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Yang,  J. S.
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Trumbull,  R.
3.1 Inorganic and Isotope Geochemistry, 3.0 Geochemistry, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Robinson,  P. T.
External Organizations;

Xiong,  F. H.
External Organizations;

Lian,  D. Y.
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3489899.pdf
(Verlagsversion), 208KB

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Zitation

Yang, J. S., Trumbull, R., Robinson, P. T., Xiong, F. H., Lian, D. Y. (2018): Comment 2 on “Ultra-high pressure and ultra-reduced minerals in ophiolites may form by lightning strikes”. - Geochemical Perspectives Letters, 8, 6-7.
https://doi.org/10.7185/geochemlet.1820


Zitierlink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_3489899
Zusammenfassung
We read with great interest the paper by C. Ballhaus and coauthors (2017) reporting on electrical discharge experiments that showed how SiC and other phases found in mantle-derived rocks can potentially form by lightning strikes (Ballhaus et al., 2017). The experiments are technically innovative and challenging and the results make fascinating reading. In a comment paper, Griffin et al. (2018) noted several lines of evidence that ultra-high pressure (UHP) and super reduced (SuR) minerals in ophiolites do not form by lightning strikes. Here, we add additional comments relating to the geological and mineralogical data from ophiolites that are not compatible with the model of Ballhaus et al. (2017).