This study examines subsurface deformation at the northern end of the Wadi Araba Fault (WAF), focusing on the Amman-Hallabat Fault (AHF) and the Wadi Shueib Fault (WSF) …
KM Ibrahim, BK Moh'd, AI Masri, MM Al-Taj… - Journal of African Earth …, 2014 - Elsevier
Abstract The E–W Siwaqa transcurrent fault is the result of tectonic activity related to the opening of the Red Sea and sinistral movement along the Dead Sea Transform (DST) …
A Batayneh, H Ghrefat, A Diabat - Journal of Earth Science, 2012 - Springer
Lineaments in the southeastern Jordan plateau are mapped using gravity data and field studies in order to understand the tectonic origin of these lineaments, especially in relation …
Organic-rich mudrocks are of great importance to the petroleum industry, potentially acting as source rocks, cap rocks or unconventional reservoirs. The analysis of natural fractures in …
Jordan is situated in the north-western corner of the Arabian plate between the stable part of the Arabian Plate and the unstable area of the Dead Sea Transform (DST). It has lateral …
Engineers of dams are often challenged by the complexity of dam locations. Some dams may be constructed close to complicated tectonic settings, where a potentially active fault …