Magma mixing in the 1100 AD Montaña Reventada composite lava flow, Tenerife, Canary Islands: Interaction between rift zone and central volcano plumbing systems

↓ Direkt till sidans innehåll
↓ Direkt till sidans sekundära innehåll (sidomenyn)

Sökning: WFRF:(Deegan Frances M) > Magma mixing in the...

LIBRIS Formathandbok (Information om MARC21)

Fältnamn	Indikatorer	Metadata
000		04298naa a2200481 4500
001		oai:DiVA.org:uu-132696
003		SwePub
008		101025s2011 \| \|\|\|\|\|\|\|\|\|\|\|000 \|\|eng\|
024	7	a https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-1326962 URI
024	7	a https://doi.org/10.1007/s00410-010-0596-x2 DOI
040		a (SwePub)uu
041		a engb eng
042		9 SwePub
072	7	a ref2 swepub-contenttype
072	7	a art2 swepub-publicationtype
100	1	a Wiesmaier, Sebastianu Department of Geology, Trinity College Dublin, 2 College Green, Dublin 2, Ireland4 aut
245	1 0	a Magma mixing in the 1100 AD Montaña Reventada composite lava flow, Tenerife, Canary Islands :b Interaction between rift zone and central volcano plumbing systems
264		c 2011-02-03
264	1	b Springer,c 2011
338		a print2 rdacarrier
500		a Erratum in: Contributions to Mineralogy and Petrology, 2011, vol. 162, pp 671-673, doi: 10.1007/s00410-011-0668-6
520		a Zoned eruption deposits commonly show a lower felsic and an upper mafic member, thought to reflect eruption from large, stratified magma chambers. In contrast, the Montaña Reventada composite flow (Tenerife) consists of a lower basanite and a much thicker upper phonolite. A sharp interface separates basanite and phonolite, and chilled margins at this contact indicate the basanite was still hot upon emplacement of the phonolite, i.e. the two magmas erupted in quick succession. Four types of mafic to intermediate inclusions are found in the phonolite. Inclusion textures comprise foamy quenched ones, others with chilled margins and yet others that are physically mingled, reflecting progressive mixing with a decreasing temperature contrast between the end-members. Analysis of basanite, phonolite and inclusions for majors, traces and Sr, Nd and Pb isotopes show the inclusions to be derived from binary mixing of basanite and phonolite end-members in ratios of 2:1 to 4:1. Although, basanite and phonolite magmas were in direct contact, contrasting 206Pb/204Pb ratios show that they are genetically distinct (19.7193(21)–19.7418(31) vs. 19.7671(18)–19.7807(23), respectively). We argue that the Montaña Reventada basanite and phonolite first met just prior to eruption and had limited interaction time only. Montaña Reventada erupted from the transition zone between two plumbing systems, the phonolitic Teide-Pico Viejo complex and the basanitic Northwest rift zone. A rift zone basanite dyke most likely intersected the previously emplaced phonolite magma chamber. This led to eruption of geochemically and texturally unaffected basanite, with the inclusion-rich phonolite subsequently following into the established conduit.
650	7	a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650	7	a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
653		a Magma mixing
653		a basanite
653		a phonolite
653		a Tenerife
653		a Canary Islands
653		a Reventada
653		a Earth sciences
653		a Geovetenskap
653		a Earth Science with specialization in Mineral Chemistry, Petrology and Tectonics
653		a Geovetenskap med inriktning mot mineralogi, petrologi och tektonik
700	1	a Deegan, Frances M,d 1983-u Uppsala universitet,Berggrundsgeologi4 aut0 (Swepub:uu)frade877
700	1	a Troll, Valentin Ru Uppsala universitet,Berggrundsgeologi4 aut0 (Swepub:uu)valtr808
700	1	a Carracedo, Juan Carlosu Estación Volcanológica de Canarias, IPNA-CSIC, Av. Astrofísica Francisco Sanchez 3, 38206 La Laguna, Tenerife, Spain4 aut
700	1	a Chadwick, Jane Pu Department of Petrology (FALW), Vrjie Universiteit, 1081 HV Amsterdam, The Netherlands4 aut
700	1	a Chew, David Mu Department of Geology, Trinity College Dublin, 2 College Green, Dublin 2, Ireland4 aut
710	2	a Department of Geology, Trinity College Dublin, 2 College Green, Dublin 2, Irelandb Berggrundsgeologi4 org
773	0	t Contributions to Mineralogy and Petrologyd : Springerg 162:3, s. 651-669q 162:3<651-669x 0010-7999x 1432-0967
856	4 8	u https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-132696
856	4 8	u https://doi.org/10.1007/s00410-010-0596-x

Hitta via bibliotek

Contributions to Mineralogy and Petrology (Sök värdpublikationen i LIBRIS)

Till lärosätets databas

Hitta mer i SwePub

Av författaren/redakt...: Wiesmaier, Sebas ...; Deegan, Frances ...; Troll, Valentin ...; Carracedo, Juan ...; Chadwick, Jane P; Chew, David M

Om ämnet

NATURVETENSKAP: NATURVETENSKAP; och Geovetenskap och ...

Artiklar i publikationen: Contributions to ...

Av lärosätet: Uppsala universitet

Sök utanför SwePub

Sök vidare i:: Google; Google Book Search; Google Scholar

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

LIBRIS.kb.se