Evidence for weak oceanic transform faults

article

Evidence for weak oceanic transform faults is …
instance of (P31):
scholarly articleQ13442814

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P819ADS bibcode2002GeoRL..29.2207B
P356DOI10.1029/2002GL015612

P50authorMaria T. ZuberQ4194276
Mark D. BehnQ53953606
P2093author name stringJian Lin
P2860cites workOceanic transverse ridges: A flexural response to fracture-zone–normal extensionQ63185008
Tectonics of ridge-transform intersections at the Kane fracture zoneQ97322328
Membrane stresses near mid-ocean ridge-transform intersectionsQ107407677
Lithospheric stress near a ridge-transform intersectionQ107407689
Focused volcanism and growth of a slow spreading segment (Mid-Atlantic Ridge, 35°N)Q57851289
The seismic moment budget of slowly spreading ridgesQ59078303
A study on the active crustal deformation of the north and east anatolian fault zonesQ60713699
P433issue24
P407language of work or nameEnglishQ1860
P304page(s)60-1-60-4
P577publication date2002-12-01
P1433published inGeophysical Research LettersQ5535576
P1476titleEvidence for weak oceanic transform faults
P478volume29

Reverse relations

cites work (P2860)
Q59705555Abyssal hill deflections at Pacific-Antarctic ridge-transform intersections
Q59799366Constraints on 3-D stress in the crust from support of mid-ocean ridge topography
Q57851736Controls on melt migration and extraction at the ultraslow Southwest Indian Ridge 10°–16°E
Q34134455Dynamical Instability Produces Transform Faults at Mid-Ocean Ridges
Q57851709Frictional behavior of oceanic transform faults and its influence on earthquake characteristics
Q57871760Skewed orientation groups in scatter plots of earthquake fault plane solutions: Implications for extensional geometry at oceanic spreading centers
Q104536147The Morphology of the Tasmantid Seamounts: Interactions Between Tectonic Inheritance and Magmatic Evolution

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