[1]
J. M. Insua-Arévalo, “Paleoseismological evidence of Holocene activity of the Los Tollos Fault (Murcia, SE Spain): A lately formed Quaternary tectonic feature of the Eastern Betic Shear Zone”, JIGE, vol. 41, no. 3, pp. 333–350, Dec. 2015, doi: https://doi.org/10.5209/rev_JIGE.2015.v41.n3.49948