Seismotectonics of the Horseshoe Abyssal Plain and Gorringe Bank, eastern Atlantic Ocean: Constraints from ocean bottom seismometer data. Issue 1 (21st January 2017)

• Record Type: Journal Article
• Authors: Grevemeyer, Ingo; Lange, Dietrich; Villinger, Heinrich; Custódio, Susana; Matias, Luis
• Is Part Of: Journal of geophysical research. Volume 122:Issue 1(2017)
• Page Start: 63
• Page End: 78
• Publication Date: 2017-01-21
• Subjects: seismotectonics -- seismic hazards -- microseismicity -- plate boundary -- Gorringe Bank -- Horseshoe Abyssal Plain; Geomagnetism -- Periodicals; Geochemistry -- Periodicals; Geophysics -- Periodicals; Earth sciences -- Periodicals; 551.1
• DOI: 10.1002/2016JB013586
• Languages: English
• ISSNs: 2169-9313

Abstract

Abstract: At the eastern end of the Azores‐Gloria transform fault system to the southwest of Portugal, the plate boundary between Africa and Iberia is a region where deformation is accommodated over a wide tectonically active area. The region has unleashed large earthquakes and tsunamis, including the Mw ~ 8.5 Great Lisbon earthquake of 1755. Although the source region of the 1755 earthquake is still disputed, most proposals include a source location in the vicinity of the Horseshoe Abyssal Plain (HAP), which is bounded by the 5000 m high Gorringe Bank (GB). In this study we characterize seismic activity in the region using data recorded by two local networks of ocean bottom seismometers. The networks were deployed in the eastern HAP and at the GB. The data set allowed the detection of 160 local earthquakes. These earthquakes cluster around the GB, to the SW of Cabo Sao Vicente, and in the HAP. Focal depths indicate deep‐seated earthquakes, with depths increasing from 20–35 km (mean of 26.1 ± 7.2 km) at the GB to 15–45 km (mean 31.5 km ± 10.5 km) under the HAP. Seismic activity thus extends down to levels that are deeper than those mapped by active seismic profiling, with the majority of events occurring within the mantle. Thermal modeling suggests that temperatures of approximately 600°C characterize the base of the seismogenic brittle lithosphere at ~45 km depth. The large source depth and thermal structure support previous suggestions that catastrophic seismic rupture through the lithospheric mantle may indeed occur in the area. Key Points: Microearthquakes occur down to 45 km and at temperatures of <600°C and rupture a domain of upper mantle, including unroofed continental mantle Seismicity occurs at depth greater than reflection seismically mapped faults, which thus may splay out from deep‐seated faults The distribution of microearthquakes do not provide any evidence for a developing subduction zone but rather indicates shortening