High transient stress in the lower crust: Evidence from dry pseudotachylytes in granulites, Lofoten Archipelago, northern Norway
Seismic activity below the standard seismogenic zone is difficult to investigate because the geological records of such earthquakes, pseudotachylytes, are typically reacted and/or deformed. Here, we describe unusually pristine pseudotachylytes in lower-crustal granulites from the Lofoten Archipelago...
Main Authors: | , , , , |
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Freie Universität Berlin
2021
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Online Access: | https://dx.doi.org/10.17169/refubium-30060 https://refubium.fu-berlin.de/handle/fub188/30320 |