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systems. The Mid-Atlantic Ridge (MAR) bends its way end is a triple junction, where it connects with the Western Volcanic Zone (WVZ) to the north via a change in strike direction, and with the South Iceland Seismic Although the quality of bathymetric data is contin-ually improving, a dearth of high-...

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Bibliographic Details
Main Author: Th Sci
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2006
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.527.30
http://www.webpages.uidaho.edu/~simkat/papers/tectonophys06.pdf
Description
Summary:systems. The Mid-Atlantic Ridge (MAR) bends its way end is a triple junction, where it connects with the Western Volcanic Zone (WVZ) to the north via a change in strike direction, and with the South Iceland Seismic Although the quality of bathymetric data is contin-ually improving, a dearth of high-resolution fracture data from mid-ocean ridges (MORs) is still an obstacle to unraveling the complex interplay between faulting