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Receiver function constraints on crustal seismic velocities and partial melting beneath the Red Sea rift and adjacent regions, Afar Depression
Author(s) -
Reed Cory A.,
Almadani Sattam,
Gao Stephen S.,
Elsheikh Ahmed A.,
Cherie Solomon,
Abdelsalam Mohamed G.,
Thurmond Allison K.,
Liu Kelly H.
Publication year - 2014
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.983
H-Index - 232
eISSN - 2169-9356
pISSN - 2169-9313
DOI - 10.1002/2013jb010719
Subject(s) - geology , rift , crust , receiver function , graben , seismology , partial melting , continental crust , lithosphere , rift zone , volcano , oceanic crust , petrology , tectonics , geophysics , subduction
The Afar Depression is an ideal locale for the investigation of crustal processes involved in the transition from continental rifting to oceanic spreading. To provide relatively high resolution images of the crust beneath the Red Sea rift (RSR) represented by the Tendaho graben in the Afar Depression, we deployed an array of 18 broadband seismic stations in 2010 and 2011. Stacking of about 2300 receiver functions from the 18 and several nearby stations along the ~200 km long array reveals an average crustal thickness of 22±4 km, ranging from ~17 km near the RSR axis to 30 km within the overlap zone between the Red Sea and Gulf of Aden rifts. The resulting anomalously high V p / V s ratios decrease from 2.40 in the southwest to 1.85 within the overlap zone. We utilize theoretical V p and melt fraction relationships to obtain an overall highly reduced average crustal V p of ~5.1 km/s. The melt percentage is about 10% beneath the RSR while the overlap zone contains minor quantities of partial melt. The observed high V p / V s values beneath most of the study area indicate widespread partial melting beneath the southwest half of the profile, probably as a result of gradual eastward migration of the RSR axis. Our results also suggest that the current extensional strain in the lower crust beneath the region is diffuse, while the strain field in the upper crust is localized along narrow volcanic segments. These disparate styles of deformation imply a high degree of decoupling between the upper and lower crust.