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Die Rolle des Gewebes bei den Reibungseigenschaften phyllosilikatreicher tektonischer Verwerfungen
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Die Rolle des Gewebes bei den Reibungseigenschaften phyllosilikatreicher tektonischer Verwerfungen

Article DOI: 10.3791/62821-v • 07:39 min • November 6th, 2021
November 6th, 2021 •
1,4, 2, 1, 1, 3, 1,3, 4, 5
1Dipartimento di Scienze della Terra, Sapienza Università di Roma, 2Dipartimento di Geoscienze, Università di Padova, 3Department of Geoscience, The Pennsylvania State University, 4Istituto Nazionale di Geofisica e Vulcanologia, 5Dipartimento di Scienze Fisiche, della Terra e dell’Ambiente, Università di Siena

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Die Reibung von phyllosilicates-reichen Fehlern, die in ihrer In-situ-Geometrie geschoren werden, ist deutlich geringer als die Reibung ihrer pulverförmigen Äquivalente.

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Environmental Sciences Tectonic faults friction fabric rock deformation experiments microstructure phyllosilicates
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