Palaeoseismic structures in Quaternary sediments, related to an assumed fault zone north of the Permian Peissen-Gnutz salt structure (NW Germany) – Neotectonic activity and earthquakes from the Saalian to the Holocene-Reference-Cited by-同舟云学术

Palaeoseismic structures in Quaternary sediments, related to an assumed fault zone north of the Permian Peissen-Gnutz salt structure (NW Germany) – Neotectonic activity and earthquakes from the Saalian to the Holocene

Published:2019-03 Issue: Volume:328 Page:15-27
ISSN:0169-555X
Container-title:Geomorphology
language:en
Short-container-title:Geomorphology

Author:

Grube Alf

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference90 articles.

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4. Reply to “Discussion on ‘Palaeoseismic structures in Quaternary sediments, related to an assumed fault zone north of the Permian Peissen-Gnutz Salt Structure (NW Germany) – Neotectonic activity and earthquakes from the Saalian to the Holocene’ (Grube, 2019)” by Pascal Bertran, Kevin Manchuel and Deborah Sicilia;Geomorphology;2021-07

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