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Oxygen isotope microanalysis of silicates with application to fluid-rock interfaces

dc.contributor.authorFiebig, Jensde
dc.date.accessioned2001-10-31T15:25:42Zde
dc.date.accessioned2013-01-18T11:25:46Zde
dc.date.available2013-01-30T23:51:05Zde
dc.date.issued2001-10-31de
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0006-B354-1de
dc.format.mimetypeapplication/pdfde
dc.language.isoengde
dc.rights.urihttp://webdoc.sub.gwdg.de/diss/copyrdiss.htmde
dc.titleOxygen isotope microanalysis of silicates with application to fluid-rock interfacesde
dc.typedoctoralThesis
dc.contributor.refereeHoefs, Jochen Prof. Dr.de
dc.date.examination2000-01-27de
dc.subject.dnb550 Geowissenschaftende
dc.description.abstractengIn order to investigate crustal fluid-rock interactions an oxygen isotope microprobe was set up. Oygen is extracted from silicates by Ultra-Violet (UV)-laser fluorination and its isotropic 18/16-ration is determined using isotope ration monitoring Gas Chromatography Mass Spectrometry (irm-GC-MS). This technique enables an accurate in situ analysis of all types of silicates, including highly transparent minerals like quartz. To reduce the influence of fluorine derived blanks on isotopic measurements, 3000 nmol oxygen is liberated, while only 30 nmol ist finally used for isotopic analysis. This way, spatial resolution is set to 250 [my]m. Precision is about 0.2o/oo, while a single analysis takes less than 15 minutes. In situ oxygen isotope- and electron microprobe analysis was addressed to a hydrothermally altered granitic pluton from the Schwarzwald, Germany. Both data sets demonstrate that an exchange of oxygen isotopes between granite and fluid occurs preferentially along microcracks. Chemical reaction and dissolution-recrystallisation are the dominant exchange mechanisms. Disequilibirium fractionations between mineral pairs, which have been obtained for the same samples by conventional ''thermal'' fluorintation on a meter-scale, are interpreted to be due to a mixing of two systems exhibiting equilibirium fractionations on a µm-scale. Large parts of the investigated granite have been intensively modified by a Na-rich fluid. On a cm-scale, oxygen isotope exchange between fluid and rock is modelled using a kinetic exchange theory. The number of preexisting microcracks drives kinetic parameters like water-rock ratio and fluid flux and thereby affects the chemical compostition of the fluid and exchange rates. This investigation confirms the hypothesis that a large fossil hydrothermal system of meteoric origin was active in the southern Schwarzwald. Due to an interaction with subsequently intruded granitic plutons the 18O depeleted meteoric fluid became continuously enrichted in 18O.de
dc.contributor.coRefereeWörner, Gerhard Prof. Dr.de
dc.subject.topicMathematics and Computer Sciencede
dc.subject.gerQuarzde
dc.subject.gerFlüssigkeitseinschlussde
dc.subject.gerSauerstoffisotopde
dc.subject.gerMirkoranalysede
dc.subject.bk38.32de
dc.identifier.urnurn:nbn:de:gbv:7-webdoc-874-9de
dc.identifier.purlwebdoc-874de
dc.affiliation.instituteFakultät für Geowissenschaften und Geographiede
dc.subject.gokfullVJC 400: Fluid-Gestein-Wechselwirkungen {Geochemie}de
dc.subject.gokfullVJJ 110: Geochemie der Stabilen Isotopende
dc.subject.gokfullVJA 240: Spektroskopische Verfahren {Geochemie}de
dc.identifier.ppn318576244


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