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- W4386242010 abstract "Abstract The Bucaramanga nest (BN) is an area of exceptionally strong intermediate-depth seismicity localized in a narrow zone at 150–170 km depth beneath the continental plate in Colombia. To explain the very unusual mantle seismicity cluster in this area, we built a seismic velocity model in the vicinity of BN with the use of local earthquake tomography and developed a numerical hydromechanical model. Our seismic model shows a strong high-velocity anomaly at 130–167 km coinciding with the BN seismicity. The relocated seismicity can be separated in two clusters. We propose that the upper BN cluster at ~ 130 km depth is attributed to dehydration embrittlement, whereas the lower BN cluster at ~ 150 km depth coinciding with the high-velocity body is caused by lithospheric delamination, creating a “drip” that falls down over the subducting oceanic plate, enhancing fluid release from the slab, potentially increasing seismicity." @default.
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- W4386242010 date "2023-08-29" @default.
- W4386242010 modified "2023-09-26" @default.
- W4386242010 title "Lithospheric Delamination as the Driving Mechanism of Intermediate-depth Seismicity in the Bucaramanga Nest, Colombia" @default.
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- W4386242010 doi "https://doi.org/10.21203/rs.3.rs-3233625/v1" @default.
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