Universität zu Köln

Ballhaus, C., Fonseca, R. O. C. and Bragagni, A. (2018). Reply to Comment on Ultra-high pressure and ultra-reduced minerals in ophiolites may form by lightning strikes by Griffin et al., 2018: No evidence for transition zone metamorphism in the Luobusa ophiolite. Geochem. Perspect. Lett., 7. S. 3 - 5. PARIS CEDEX 05: EUROPEAN ASSOC GEOCHEMISTRY. ISSN 2410-3403

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Item Type:	Journal Article
Creators:	Creators Email ORCID ORCID Put Code Ballhaus, C. UNSPECIFIED UNSPECIFIED UNSPECIFIED Fonseca, R. O. C. UNSPECIFIED UNSPECIFIED UNSPECIFIED Bragagni, A. UNSPECIFIED UNSPECIFIED UNSPECIFIED
URN:	urn:nbn:de:hbz:38-200433
DOI:	10.7185/geochemlet.1810
Journal or Publication Title:	Geochem. Perspect. Lett.
Volume:	7
Page Range:	S. 3 - 5
Date:	2018
Publisher:	EUROPEAN ASSOC GEOCHEMISTRY
Place of Publication:	PARIS CEDEX 05
ISSN:	2410-3403
Language:	English
Faculty:	Unspecified
Divisions:	Unspecified
Subjects:	no entry
Uncontrolled Keywords:	Keywords Language SILICATE LIQUID; CHROMITITES; DIAMONDS; COESITE; SPINEL; TIBET Multiple languages Geochemistry & Geophysics Multiple languages
Refereed:	Yes
URI:	http://kups.ub.uni-koeln.de/id/eprint/20043