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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F12%3A10128655%21RIV13-GA0-11310___
rdf:type
skos:Concept n3:Vysledek
rdfs:seeAlso
http://dx.doi.org/10.1016/j.gr.2011.09.013
dcterms:description
The Blue Mountains Province of northeastern Oregon, western Idaho, and southeastern Washington (USA) consists of the amalgamated Wallowa distal island arc, Baker melange-bearing accretionary wedge-forearc, and Olds Ferry fringing island arc terranes. Anisotropy of magnetic susceptibility (AMS) and particularly the orientation of magnetic lineations in Middle to Late Jurassic diorite-tonalite-granodiorite plutons intruding the Baker terrane indicate a change in tectonic regime from flattening with principal stretching at a high angle to the local orientation of the terrane boundaries at around 160 Ma to constriction with boundary-subparallel subhorizontal stretching at ca. 146 Ma. The former magnetic fabric is compatible with magnetic lineations recording strain related to top-to-the-southwest back-thrusting onto the Olds Ferry arc. In contrast, the similar to 146 Ma boundary-parallel stretching may record strain partitioning whereby a part of the Baker terrane was extruded laterally parallel to terrane boundaries after the terrane collision. After restoration for the clockwise post-mid-Cretaceous terrane rotation, the similar to 160 Ma restored principal stretching directions are compatible with the overall left-oblique subduction and convergence of the Wallowa distal and Olds Ferry fringing arc terranes. Magnetic fabric data from the plutons thus support the interpretation that the early displacement of the Blue Mountains Superterrane, and perhaps also its possible correlative Intermontane Superterrane of the Canadian Cordillera, was southward along the truncated North American continental margin during the late Middle Jurassic. The Blue Mountains Province of northeastern Oregon, western Idaho, and southeastern Washington (USA) consists of the amalgamated Wallowa distal island arc, Baker melange-bearing accretionary wedge-forearc, and Olds Ferry fringing island arc terranes. Anisotropy of magnetic susceptibility (AMS) and particularly the orientation of magnetic lineations in Middle to Late Jurassic diorite-tonalite-granodiorite plutons intruding the Baker terrane indicate a change in tectonic regime from flattening with principal stretching at a high angle to the local orientation of the terrane boundaries at around 160 Ma to constriction with boundary-subparallel subhorizontal stretching at ca. 146 Ma. The former magnetic fabric is compatible with magnetic lineations recording strain related to top-to-the-southwest back-thrusting onto the Olds Ferry arc. In contrast, the similar to 146 Ma boundary-parallel stretching may record strain partitioning whereby a part of the Baker terrane was extruded laterally parallel to terrane boundaries after the terrane collision. After restoration for the clockwise post-mid-Cretaceous terrane rotation, the similar to 160 Ma restored principal stretching directions are compatible with the overall left-oblique subduction and convergence of the Wallowa distal and Olds Ferry fringing arc terranes. Magnetic fabric data from the plutons thus support the interpretation that the early displacement of the Blue Mountains Superterrane, and perhaps also its possible correlative Intermontane Superterrane of the Canadian Cordillera, was southward along the truncated North American continental margin during the late Middle Jurassic.
dcterms:title
Magnetic fabric of Late Jurassic arc plutons and kinematics of terrane accretion in the Blue Mountains, northeastern Oregon Magnetic fabric of Late Jurassic arc plutons and kinematics of terrane accretion in the Blue Mountains, northeastern Oregon
skos:prefLabel
Magnetic fabric of Late Jurassic arc plutons and kinematics of terrane accretion in the Blue Mountains, northeastern Oregon Magnetic fabric of Late Jurassic arc plutons and kinematics of terrane accretion in the Blue Mountains, northeastern Oregon
skos:notation
RIV/00216208:11310/12:10128655!RIV13-GA0-11310___
n3:predkladatel
n4:orjk%3A11310
n5:aktivita
n13:Z n13:P n13:I
n5:aktivity
I, P(GP205/07/P226), Z(MSM0021620855)
n5:cisloPeriodika
1
n5:dodaniDat
n8:2013
n5:domaciTvurceVysledku
n14:8387699 n14:2387689
n5:druhVysledku
n15:J
n5:duvernostUdaju
n9:S
n5:entitaPredkladatele
n21:predkladatel
n5:idSjednocenehoVysledku
147753
n5:idVysledku
RIV/00216208:11310/12:10128655
n5:jazykVysledku
n17:eng
n5:klicovaSlova
terrane accretion; North American craton; Blue Mountains Province; Baker terrane; Anisotropy of magnetic susceptibility (AMS)
n5:klicoveSlovo
n6:Baker%20terrane n6:Blue%20Mountains%20Province n6:North%20American%20craton n6:Anisotropy%20of%20magnetic%20susceptibility%20%28AMS%29 n6:terrane%20accretion
n5:kodStatuVydavatele
JP - Japonsko
n5:kontrolniKodProRIV
[9BAE6A139D44]
n5:nazevZdroje
Gondwana Research
n5:obor
n22:DB
n5:pocetDomacichTvurcuVysledku
2
n5:pocetTvurcuVysledku
4
n5:projekt
n20:GP205%2F07%2FP226
n5:rokUplatneniVysledku
n8:2012
n5:svazekPeriodika
22
n5:tvurceVysledku
Johnson, Kenneth Verner, Kryštof Žák, Jiří Schwartz, Joshua J.
n5:wos
000305106800026
n5:zamer
n19:MSM0021620855
s:issn
1342-937X
s:numberOfPages
12
n18:doi
10.1016/j.gr.2011.09.013
n11:organizacniJednotka
11310