Faulting Intersections and Magma-feeding Zones in Tihamat-Asir, Southeast Red Sea Rift: Aeromagnetic and Structural Perspective

مقال فى مجلة

2021

تم النشر فى: https://doi.org/10.1016/j.jafrearsci.2020.104044

The Tihamat-Asir area is located in southwest Saudi Arabia between the Asir Mountains and the Red Sea coast.
Herein, the Tihamat-Asir area aeromagnetic data are re-interpreted to explain the magmatic activity and related
structural interaction between extensional normal and transfer strike-slip faulting. The magnetic anomaly
structural interpretation indicates that faulting and related magmatic activities are the main structural features
affecting the study area. The magnetic signatures reveal oceanic crust underlying the onshore and offshore
western side of the study area, while the eastern side is characterized by a broad, low magnetic anomaly
indicative of continental crust. The boundary between the oceanic and continental crusts is not sharp, and
represents a transitional zone, characterized by magnetic gradient steepness potentially related to mid-Cenozoic
gabbroic plutons and volcanic flows together with normal faults injected by Cenozoic basalts. This zone incorporates
three NW striking normal faulting and NE striking transfer strike-slip faulting system intersections,
located close to Baysh, Abu Arish, and southwest of Abu Arish. The intersectional interactions between these two
faulting systems have resulted in brittle magma-feeding zones that have allowed magma to reach the surface at
these localities, and is believed to have resulted from the fracturing process affecting these localities due to the
accumulated stress exerted by the movement of the NE strike-slip faults along the normal NW faulting systems
and the associated releasing bends. A pull-apart magma-feeding zone is the structural model proposed to explain
the interpreted brittle magma feeding zones and the associated magmatic activities in the study area.