Magnetic fabric of Plio-Pleistocene clayey sediments from the footwall of the Avezzano eathquake fault (central Appennines, Italy). AMQ [Internet]. 2024 May 17 [cited 2024 Nov. 23];9(1):145-54. Available from: https://amq.aiqua.it/index.php/amq/article/view/1085