History of faulting and magmatism in the Galilee (Israel) and across the Levant continental margin inferred from potential field data

▶ Rehovot-Carmel N-S RTP anomaly, Gaash high and Pleshet graben, represent Perm-Trias structures. ▶ Jonah Ridge and Beirut SW-NE RTP anomalies delineate the Levant continental edge. ▶ Jurassic volcanics have negative RTP anomalies and negative RR gravity anomalies. ▶ Carmel fault propagated during the Senonian from the Levant basin toward Azraq-Sirhan graben. ▶ Oligocene NW propagation of Azraq-Sirhan structure terminated ∼10 km west of the present DST.