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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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Format: | Text |
Language: | English |
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2006
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.527.30 http://www.webpages.uidaho.edu/~simkat/papers/tectonophys06.pdf |
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 |
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