Three-dimensional seismic structure of a Mid-Atlantic Ridge segment characterized by active detachment faulting (Trans-Atlantic Geotraverse, 25°55′N-26°20′N)

We use air gun shots recorded by ocean bottom seismometers (OBSs) to generate a three‐dimensional (3D)P‐wave tomographic velocity model of the Trans‐Atlantic Geotraverse (TAG) segment of the Mid‐Atlantic Ridge, and to search for evidence of reflections from a shallow crustal fault interface. Near‐ve...

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Veröffentlicht in:	Geochemistry, geophysics, geosystems : G3 geophysics, geosystems : G3, 2012-11, Vol.13 (11), p.np-n/a
Hauptverfasser:	Zhao, Minghui, Canales, Juan Pablo, Sohn, Robert A.
Format:	Artikel
Sprache:	eng
Schlagworte:	3D seismic structure active detachment fault Anomalies Circulation Detachment Footwalls Mid-Atlantic Ridge Ocean floor Reflection Ridges Segments TAG hydrothermal field Three dimensional Velocity Wave velocity
Online-Zugang:	Volltext
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