a ar

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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Main Author: Th Sci
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2006
Subjects:
Mid-Atlantic Ridge
Iceland
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.527.30
http://www.webpages.uidaho.edu/~simkat/papers/tectonophys06.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.527.30 2023-05-15T16:47:27+02:00 a ar Th Sci The Pennsylvania State University CiteSeerX Archives 2006 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.527.30 http://www.webpages.uidaho.edu/~simkat/papers/tectonophys06.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.527.30 http://www.webpages.uidaho.edu/~simkat/papers/tectonophys06.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.webpages.uidaho.edu/~simkat/papers/tectonophys06.pdf text 2006 ftciteseerx 2016-01-08T10:24:48Z 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 Text Iceland Unknown Mid-Atlantic Ridge
institution Open Polar
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language English
description 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
author2 The Pennsylvania State University CiteSeerX Archives
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publishDate 2006
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.527.30
http://www.webpages.uidaho.edu/~simkat/papers/tectonophys06.pdf
geographic Mid-Atlantic Ridge
geographic_facet Mid-Atlantic Ridge
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op_source http://www.webpages.uidaho.edu/~simkat/papers/tectonophys06.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.527.30
http://www.webpages.uidaho.edu/~simkat/papers/tectonophys06.pdf
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