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Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F10%3A00000518%21RIV14-MSM-00025798
rdf:type
skos:Concept n16:Vysledek
rdfs:seeAlso
http://link.springer.com/article/10.1007%2Fs00531-009-0423-7
dcterms:description
The Tuolumne batholith, Sierra Nevada, California, consists of several nested granitoid units and is an example of upper-crustal normally zoned intrusions. The two outermost units of the batholith are separated by a wide gradational contact in what is interpreted to represent a large magma chamber. In the Potter Point area near the eastern margin of the batholith, the gradational contact is cross-cut by a network of interconnected mafic–felsic sheets, which grade into zones of magmatic erosion by stoping where the host granodiorite between the sheets was entirely removed and replaced by younger enclave-rich quartz diorite. We interpret these features to record disruption of a steep solidification front, which migrated inwards from the eastern batholith margin and separated the mushy to solidified margin from the remaining active magma chamber. When intersecting the gradational contact, the solidification front started to break up via a network of tectonically driven fractures accompanied by simultaneous injection of localized magma pulses. The solidification front break-up is interpreted here as an initial stage of a “recycling” process, whereby older magma mush is disrupted and incorporated into younger magma batches, a process we propose to have been widespread along internal contacts in the Tuolumne magma chamber. The Tuolumne batholith, Sierra Nevada, California, consists of several nested granitoid units and is an example of upper-crustal normally zoned intrusions. The two outermost units of the batholith are separated by a wide gradational contact in what is interpreted to represent a large magma chamber. In the Potter Point area near the eastern margin of the batholith, the gradational contact is cross-cut by a network of interconnected mafic–felsic sheets, which grade into zones of magmatic erosion by stoping where the host granodiorite between the sheets was entirely removed and replaced by younger enclave-rich quartz diorite. We interpret these features to record disruption of a steep solidification front, which migrated inwards from the eastern batholith margin and separated the mushy to solidified margin from the remaining active magma chamber. When intersecting the gradational contact, the solidification front started to break up via a network of tectonically driven fractures accompanied by simultaneous injection of localized magma pulses. The solidification front break-up is interpreted here as an initial stage of a “recycling” process, whereby older magma mush is disrupted and incorporated into younger magma batches, a process we propose to have been widespread along internal contacts in the Tuolumne magma chamber.
dcterms:title
Magmatic erosion of the solidification front during reintrusion: the eastern margin of the Tuolumne batholith, Sierra Nevada, California Magmatic erosion of the solidification front during reintrusion: the eastern margin of the Tuolumne batholith, Sierra Nevada, California
skos:prefLabel
Magmatic erosion of the solidification front during reintrusion: the eastern margin of the Tuolumne batholith, Sierra Nevada, California Magmatic erosion of the solidification front during reintrusion: the eastern margin of the Tuolumne batholith, Sierra Nevada, California
skos:notation
RIV/00025798:_____/10:00000518!RIV14-MSM-00025798
n5:aktivita
n12:Z n12:I n12:P
n5:aktivity
I, P(GP205/07/P226), Z(MSM0021620855)
n5:cisloPeriodika
4
n5:dodaniDat
n15:2014
n5:domaciTvurceVysledku
n13:8387699
n5:druhVysledku
n14:J
n5:duvernostUdaju
n9:S
n5:entitaPredkladatele
n17:predkladatel
n5:idSjednocenehoVysledku
269140
n5:idVysledku
RIV/00025798:_____/10:00000518
n5:jazykVysledku
n20:eng
n5:klicovaSlova
Granite, Magma chamber, Magmatic stoping, Pluton, Sierra Nevada, Solidification front
n5:klicoveSlovo
n6:Magma%20chamber n6:Solidification%20front n6:Magmatic%20stoping n6:Pluton n6:Granite n6:Sierra%20Nevada
n5:kodStatuVydavatele
DE - Spolková republika Německo
n5:kontrolniKodProRIV
[C8A428F41039]
n5:nazevZdroje
International Journal of Earth Sciences
n5:obor
n19:DB
n5:pocetDomacichTvurcuVysledku
1
n5:pocetTvurcuVysledku
2
n5:projekt
n10:GP205%2F07%2FP226
n5:rokUplatneniVysledku
n15:2010
n5:svazekPeriodika
99
n5:tvurceVysledku
Paterson, Scott Žák, Jiří
n5:wos
000277641600006
n5:zamer
n18:MSM0021620855
s:issn
1437-3254
s:numberOfPages
12
n11:doi
10.1007/s00531-009-0423-7