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Internal structure of the oceanic lithosphere at a melt‐starved ultra‐slow‐spreading mid‐ocean ridge: insights from 2‐D seismic data ArchiMer
Momoh, Ekeabino; Cannat, Mathilde; Leroy, Sylvie.
Extensive outcrops of serpentinized peridotite in melt‐starved spreading corridors of the ultraslow easternmost Southwest Indian Ridge are hypothesized to be due to slip on successive long‐offset normal faults that alternate polarity (flip‐flop detachment faults). We investigate the nature of the oceanic crust which forms under these conditions, using seismic reflection data acquired during the SISMOSMOOTH 2014 cruise. Using 3‐D binning, the seismic profiles were binned elastically, while three of the profiles shot closely were merged into one to take advantage of the larger air gun source volume. Using a poststack imaging sequence, we observe several types of reflectors at crustal and infracrustal depths, in the axial valley and off‐axis. Correlating our...
Tipo: Text Palavras-chave: Detachment faulting; Ultra-slow spreading; Serpentinization.
Ano: 2020 URL: https://archimer.ifremer.fr/doc/00599/71124/69429.pdf
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Quasi-3D seismic reflection imaging, and wide-angle velocity structure of nearly amagmatic oceanic lithosphere at the ultra-slow spreading Southwest Indian Ridge ArchiMer
Momoh, Ekeabino; Cannat, Mathilde; Watremez, Louise; Leroy, Sylvie; Singh, Satish C..
We present results from 3D processing of 2D seismic data shot along 100 m-spaced profiles in a 1.8 km wide by 24 km long box during the SISMOSMOOTH 2014 cruise. The study is aimed at understanding the oceanic crust formed at an end-member mid-ocean ridge environment of nearly zero melt supply. Three distinct packages of reflectors are imaged: (1) south-facing reflectors which we propose correspond to the damage zone induced by the active axial detachment fault. Reflectors in the damage zone have dips up to 60° and are visible down to 5 km below the seafloor; (2) series of north-dipping reflectors in the hanging wall of the detachment fault. These reflectors may correspond to damage zone inherited from a previous, north-dipping detachment fault, or small...
Tipo: Text Palavras-chave: Amagmatic; Ultraslow mid-ocean ridge; 3-D seismic; Tomography; Detachment fault; Damage zone.
Ano: 2017 URL: https://archimer.ifremer.fr/doc/00411/52215/52943.pdf
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