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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F12%3A10128648%21RIV13-MSM-11310___
rdf:type
skos:Concept n18:Vysledek
rdfs:seeAlso
http://dx.doi.org/10.1017/S0954102011000599
dcterms:description
At Pitt Point, the east coast of Graham Land (Antarctic Peninsula), the Early to Middle Jurassic (Toarcian-Aalenian) rhyolite dykes form two coevally emplaced NNE-SSW and E-W trending sets. The nearly perpendicular dyke sets define a large-scale chocolate-tablet structure, implying biaxial principal extension in the WNW-ESE and N-S directions. Along the nearby north-eastern slope of Mount Reece, the WNW-ESE set locally dominates suggesting variations in the direction and amount of extension. Magnetic fabric in the dykes, revealed using the anisotropy of magnetic susceptibility (AMS) method, indicates dip-parallel to dip-oblique (?upward) magma flow. The dykes are interpreted as representing sub-volcanic feeder zones above a felsic magma source. The dyke emplacement was synchronous with the initial stages of the Weddell Sea opening during Gondwana break-up, but it remains unclear whether it was driven by regional stress field, local stress field above a larger plutonic body, or by an interaction of both. At Pitt Point, the east coast of Graham Land (Antarctic Peninsula), the Early to Middle Jurassic (Toarcian-Aalenian) rhyolite dykes form two coevally emplaced NNE-SSW and E-W trending sets. The nearly perpendicular dyke sets define a large-scale chocolate-tablet structure, implying biaxial principal extension in the WNW-ESE and N-S directions. Along the nearby north-eastern slope of Mount Reece, the WNW-ESE set locally dominates suggesting variations in the direction and amount of extension. Magnetic fabric in the dykes, revealed using the anisotropy of magnetic susceptibility (AMS) method, indicates dip-parallel to dip-oblique (?upward) magma flow. The dykes are interpreted as representing sub-volcanic feeder zones above a felsic magma source. The dyke emplacement was synchronous with the initial stages of the Weddell Sea opening during Gondwana break-up, but it remains unclear whether it was driven by regional stress field, local stress field above a larger plutonic body, or by an interaction of both.
dcterms:title
Magnetic fabric and tectonic setting of the Early to Middle Jurassic felsic dykes at Pitt Point and Mount Reece, eastern Graham Land, Antarctica Magnetic fabric and tectonic setting of the Early to Middle Jurassic felsic dykes at Pitt Point and Mount Reece, eastern Graham Land, Antarctica
skos:prefLabel
Magnetic fabric and tectonic setting of the Early to Middle Jurassic felsic dykes at Pitt Point and Mount Reece, eastern Graham Land, Antarctica Magnetic fabric and tectonic setting of the Early to Middle Jurassic felsic dykes at Pitt Point and Mount Reece, eastern Graham Land, Antarctica
skos:notation
RIV/00216208:11310/12:10128648!RIV13-MSM-11310___
n18:predkladatel
n19:orjk%3A11310
n3:aktivita
n8:Z n8:P
n3:aktivity
P(SPII1A9/23/07), Z(MSM0021620855)
n3:cisloPeriodika
1
n3:dodaniDat
n22:2013
n3:domaciTvurceVysledku
n13:8387699
n3:druhVysledku
n14:J
n3:duvernostUdaju
n11:S
n3:entitaPredkladatele
n16:predkladatel
n3:idSjednocenehoVysledku
147752
n3:idVysledku
RIV/00216208:11310/12:10128648
n3:jazykVysledku
n17:eng
n3:klicovaSlova
Trinity Peninsula Group; regional extension; Gondwana break-up; Chon Aike silicic large igneous province; Antarctic peninsula; Anisotropy of magnetic susceptibility (AMS)
n3:klicoveSlovo
n4:Gondwana%20break-up n4:Trinity%20Peninsula%20Group n4:Antarctic%20peninsula n4:Anisotropy%20of%20magnetic%20susceptibility%20%28AMS%29 n4:Chon%20Aike%20silicic%20large%20igneous%20province n4:regional%20extension
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[E14E225AB268]
n3:nazevZdroje
Antarctic Science
n3:obor
n21:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
4
n3:projekt
n12:SPII1A9%2F23%2F07
n3:rokUplatneniVysledku
n22:2012
n3:svazekPeriodika
24
n3:tvurceVysledku
Soejono, Igor Žák, Jiří Venera, Zdeněk Janoušek, Vojtěch
n3:wos
000299936300007
n3:zamer
n15:MSM0021620855
s:issn
0954-1020
s:numberOfPages
14
n20:doi
10.1017/S0954102011000599
n5:organizacniJednotka
11310