000165798 001__ 165798
000165798 005__ 20260114135812.0
000165798 0247_ $$2doi$$a10.1016/j.lithos.2011.11.012
000165798 0248_ $$2sideral$$a76265
000165798 037__ $$aART-2012-76265
000165798 041__ $$aeng
000165798 100__ $$0(orcid)0000-0002-2944-8736$$aUbide, T.
000165798 245__ $$aThe influence of crystal settling on the compositional zoning of a thin lamprophyre sill: A multi-method approach
000165798 260__ $$c2012
000165798 5203_ $$aWe have studied a visibly zoned, thin (< 0.5 m) lamprophyre sill that crops out in the Catalonian Coastal Ranges (NE Spain). The sill is a camptonite composed of large abundant crystals, mainly of clinopyroxene and amphibole, set in a fine-grained groundmass. The mineral chemistry of the different crystal populations indicates that the large crystals are inherited antecrysts incorporated into the magma before emplacement. The major and trace element whole rock profiles are S-shaped, with the development of a marginal reversal in the lower chilled margin. These profiles cannot be explained by normal fractionation of the magma inwards. Instead, the whole rock zoning is controlled by the presence of antecrysts. This is proven: 1) quantitatively, through a trace element model which evaluates the contribution of the antecrysts to the overall composition of the rock, and 2) statistically, through a principal component analysis on the complete trace element data set. The mineral and groundmass compositions show rectilinear compositional profiles, indicating that the magma was emplaced in a single pulse. The accumulation of the antecrysts towards the bottom of the sill, together with the calculation of settling velocities for clinopyroxene and amphibole and cooling velocities for the magma, indicate that the settling of antecrysts during cooling is responsible for the varying proportions of antecrysts and therefore for the whole rock compositional zoning. This study proves that crystal settling is a significant process in triggering compositional zoning of igneous intrusions even at the cm-scale, provided that the magma carries large crystals upon emplacement.
000165798 536__ $$9info:eu-repo/grantAgreement/ES/MICINN/CGL2008-06098-BTE
000165798 540__ $$9info:eu-repo/semantics/closedAccess$$aAll rights reserved$$uhttp://www.europeana.eu/rights/rr-f/
000165798 590__ $$a3.779$$b2012
000165798 591__ $$aMINERALOGY$$b1 / 26 = 0.038$$c2012$$dQ1$$eT1
000165798 591__ $$aGEOCHEMISTRY & GEOPHYSICS$$b7 / 76 = 0.092$$c2012$$dQ1$$eT1
000165798 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000165798 700__ $$0(orcid)0000-0002-0710-9178$$aArranz, E.$$uUniversidad de Zaragoza
000165798 700__ $$0(orcid)0000-0002-3609-7380$$aLago, M.$$uUniversidad de Zaragoza
000165798 700__ $$0(orcid)0000-0002-2745-0357$$aGalé, C.$$uUniversidad de Zaragoza
000165798 700__ $$0(orcid)0000-0001-8470-2840$$aLarrea, P.$$uUniversidad de Zaragoza
000165798 7102_ $$12000$$2685$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Petrología y Geoquímica
000165798 773__ $$g132-133 (2012), 37-49$$pLithos$$tLITHOS$$x0024-4937
000165798 8564_ $$s1638055$$uhttps://zaguan.unizar.es/record/165798/files/texto_completo.pdf$$yVersión publicada
000165798 8564_ $$s2949300$$uhttps://zaguan.unizar.es/record/165798/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000165798 909CO $$ooai:zaguan.unizar.es:165798$$particulos$$pdriver
000165798 951__ $$a2026-01-14-12:45:59
000165798 980__ $$aARTICLE