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Statements

Subject Item
n2:RIV%2F00025798%3A_____%2F09%3A00000538%21RIV14-MSM-00025798
rdf:type
n16:Vysledek skos:Concept
rdfs:seeAlso
http://journals.cambridge.org/action/displayAbstract?fromPage=online&aid=7834142
dcterms:description
The causes of compositional diversity in the Tuolumne Batholith, whether source heterogeneity, magma mixing, or fractional crystallisation, is a matter of longstanding debate. This paper presents data from detailed mapping and a microstructural and major element, trace element and isotopic study of an elongate lobe of the Half Dome granodiorite that protrudes from the southern end of the batholith. The lobe is normally zoned from quartz diorite along the outer margin to high-silica leucogranite in the core. Contacts are steep and gradational, except for the central leucogranite contact, which is locally sharp: magmatic fabrics overprint contacts. A striking feature of the lobe is the 18 wt SiO2 range comparable to that observed for the entire Tuolumne Batholith. Feldspar-compatible elements (Sr and Ba) decrease towards the centre, while Rb increases. Light and middle REEs show a smooth decrease towards the centre of the lobe. Calculated initial isotopic ratios of 87Sr/86Sr(i) and The causes of compositional diversity in the Tuolumne Batholith, whether source heterogeneity, magma mixing, or fractional crystallisation, is a matter of longstanding debate. This paper presents data from detailed mapping and a microstructural and major element, trace element and isotopic study of an elongate lobe of the Half Dome granodiorite that protrudes from the southern end of the batholith. The lobe is normally zoned from quartz diorite along the outer margin to high-silica leucogranite in the core. Contacts are steep and gradational, except for the central leucogranite contact, which is locally sharp: magmatic fabrics overprint contacts. A striking feature of the lobe is the 18 wt SiO2 range comparable to that observed for the entire Tuolumne Batholith. Feldspar-compatible elements (Sr and Ba) decrease towards the centre, while Rb increases. Light and middle REEs show a smooth decrease towards the centre of the lobe. Calculated initial isotopic ratios of 87Sr/86Sr(i) and
dcterms:title
Causes of compositional diversity in a lobe of the Half Dome granodiorite, Tuolumne Batholith, Central Sierra Nevada, California Causes of compositional diversity in a lobe of the Half Dome granodiorite, Tuolumne Batholith, Central Sierra Nevada, California
skos:prefLabel
Causes of compositional diversity in a lobe of the Half Dome granodiorite, Tuolumne Batholith, Central Sierra Nevada, California Causes of compositional diversity in a lobe of the Half Dome granodiorite, Tuolumne Batholith, Central Sierra Nevada, California
skos:notation
RIV/00025798:_____/09:00000538!RIV14-MSM-00025798
n3:aktivita
n4:I n4:P n4:Z
n3:aktivity
I, P(KJB3111403), Z(MSM0021620855)
n3:cisloPeriodika
spec. issue 1-2
n3:dodaniDat
n10:2014
n3:domaciTvurceVysledku
n6:8387699
n3:druhVysledku
n19:J
n3:duvernostUdaju
n12:S
n3:entitaPredkladatele
n14:predkladatel
n3:idSjednocenehoVysledku
249767
n3:idVysledku
RIV/00025798:_____/09:00000538
n3:jazykVysledku
n20:eng
n3:klicovaSlova
fractional crystallisation, magmatic processes, plutons
n3:klicoveSlovo
n9:magmatic%20processes n9:plutons n9:fractional%20crystallisation
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[6C9B38C0A9DB]
n3:nazevZdroje
Earth and Environmental Science Transactions of the Royal Society of Edinburgh
n3:obor
n17:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
6
n3:projekt
n15:KJB3111403
n3:rokUplatneniVysledku
n10:2009
n3:svazekPeriodika
100
n3:tvurceVysledku
Erdmann, Saskia Paterson, Scott Žák, Jiří Miller, Jonathan Memeti, Valbone Economos, Rita
n3:wos
000284505000013
n3:zamer
n18:MSM0021620855
s:issn
1755-6910
s:numberOfPages
11
n5:doi
10.1017/S1755691009016065