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Ultra-high pressure and ultra-reduced minerals in ophiolites may form by lightning strikesAffiliations | Corresponding Author | Cite as | Funding information
1Steinmann Institute, University of Bonn, Germany
2Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, Germany
3Wehrtechnische Dienststelle, WTD 81, Greding, Germany
4Institute of Geology and Mineralogy, University of Cologne, Germany
5Department of Geoscience, University of Århus, Denmark
6Fraunhofer Institute for Building Physics Holzkirchen, Germany
Ballhaus, C., Wirth, R., Fonseca, R.O.C., Blanchard, H., Pröll, W., Bragagni, A., Nagel, T., Schreiber, A., Dittrich, S., Thome, V., Hezel, D.C., Below, R., Cieszynski, H. (2017) Ultra-high pressure and ultra-reduced minerals in ophiolites may form by lightning strikes. Geochem. Persp. Let. 5, 42–46.
German Research Council (DFG).