Davies, R. J. and MacLeod, C. J. and Morgan, R. and Briggs, S. E. (2005) 'Termination of a fossil continent-ocean fracture zone imaged with three-dimensional seismic data : the Chain Fracture Zone, eastern Equatorial Atlantic.', Geology., 33 (8). pp. 641-644.
We describe the first three-dimensional imaging of the termination of a continent-ocean fracture zone (COFZ), the Chain Fracture Zone, located offshore of the Niger Delta. The COFZ marks the abrupt transition between extended continental crust, comprising multiple half-graben, and oceanic crust that has a pervasive seafloor-spreading fabric. It preserves a history of continent-continent shearing followed by oceanic crust accretion and continent-ocean shearing during the inception of Atlantic rifting. The termination is marked by steeply dipping faults with sigmoidal planform and thrusts that probably formed as a result of continent-continent or continent-ocean shearing. These are crosscut by the seafloor-spreading fabric that formed during the subsequent phase of oceanic crust accretion. The accreted oceanic crust is cut by listric and planar faults that curve in the direction of the COFZ, where they terminate. The transition from continental to oceanic crust across the COFZ is sharp and resolvable to 100–200 m. Complexes of lava flows emanate from volcanoes along the COFZ, bifurcating and trifurcating down the volcano flanks. The volcanoes are 2–5.5 km wide and 1.4 km in height relative to adjacent oceanic crust and were injected at the COFZ, probably as the spreading center migrated along it.
|Additional Information:||Geological Society of America, P.O. Box 9140, Boulder, CO 80301-9140 USA (http://www.geosociety.org)|
|Keywords:||Seismic reflection, Fracture zone, Transitional crust, Oceanic crust.|
|Full text:||Full text not available from this repository.|
|Publisher Web site:||http://dx.doi.org/10.1130/G21530.1|
|Record Created:||19 Jul 2007|
|Last Modified:||08 Feb 2011 16:36|
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