Magnetic fabric of Plio-Pleistocene clayey sediments from the footwall of the Avezzano eathquake fault (central Appennines, Italy). Alpine and Mediterranean Quaternary, [S. l.], v. 9, n. 1, p. 145–154, 2024. DOI: 10.26382/. Disponível em: https://amq.aiqua.it/index.php/amq/article/view/1085.. Acesso em: 16 jul. 2024.