作者: F. Zwaan , G. Corti , F. Sani , D. Keir , A. A. Muluneh
DOI: 10.1029/2019TC006043
关键词:
摘要: The Afar region in East Africa represents a key location to study continental breakup. We present an integrated structural analysis of the Western Margin (WAM) aiming better understand rifted margin development and role plate rotation during rifting. New information from remote sensing, fieldwork, earthquake data sets reveals that N‐S striking WAM is still actively deforming characterized by NNW‐SSE normal faulting as well series marginal grabens. Seismicity distribution first‐ever borehole‐calibrated sections this developing passive show recent slip concentrated along antithetic faults. Tectonic stress parameters derived focal mechanisms reveal different extension directions (82°N), (66°N) Main Ethiopian Rift (108°N). Fault yields same direction. Combined with GPS data, shows current tectonics dominated local Danakil Block, considered have occurred since 11 Ma. Earlier stages (since 31–25 Ma) were most likely related large‐scale Arabian plate. Various authors proposed scenarios for evolution WAM. Any complete model should consider, among other factors, multiphase tectonic history fault activity margin. findings are not only relevant understanding but also provide insights into rotational rifting formation general.