Modelling changes in stable isotope compositions of minerals during net transfer reactions in a contact aureole: Wollastonite growth at the northern Hunter Mountain Batholith (Death Valley National Park, USA)

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• 作者：Susanne  ; Skorap> ;   ; p>p>ap>p> ;   ; p>p>Susanne.Skora@bristol.ac.ukp> ; Lukas P.  ; Baumgartnerp>ap>p> ;   ; p>p>Lukas.Baumgartner@unil.chp> ; Torsten W.  ; Vennemannp>ap>p> ;   ; p>p>Torsten.Vennemann@unil.chp>
• 关键词：Wollastonite ; Contact metamorphism ; Fluid flow ; Stable isotopes ; Fractionation ; Hunter Mountain Batholith
• 刊名：Chemical Geology
• 出版年：2011
• 出版时间：23 October 2011
• 年：2011
• 卷：289
• 期：3-4
• 页码：197-209
• 全文大小：6626 K

文摘

One of the world's largest wollastonite deposits was formed at the contact of the northern Hunter Mountain Batholith (California, USA) in Paleozoic sediments. Wollastonite occurs as zones of variable thickness surrounding layers or nodules of quartzite in limestones. A minimum formation temperature of 650 ¡ãC is estimated from isolated periclase-bearing lenses in that area. Contact metamorphism of siliceous carbonates has produced mineral assemblages that are consistent with heterogeneous, and partly limited infiltration of water-rich fluids, compatible with p xmlns="""">18p>O/p xmlns="""">16p>O and p xmlns="""">13p>C/p xmlns="""">12p>C isotopic patterns recorded in carbonates.<p>Oxygen isotope compositions of wollastonites in the study area may also not require infiltration of large quantities of externally-derived fluids that were out of equilibrium with the rocks. ¦Äp xmlns="""">18p>O values of wollastonite are high (14.8?to 25.0? median: 19.7? and close to those of the host limestone (19.7?to 28? median: 24.9? and quartz (18.0?to 29.1? median: 22.6?. Isotopic disequilibrium exists at quartz/wollastonite and wollastonite/calcite boundaries. Therefore, classical batch/Rayleigh fractionation models based on reactant and product equilibrium are not applicable to the wollastonite rims. An approach that relies on local instantaneous mass balance for the reactants, based on the wollastonite-forming reaction is suggested as an alternative way to model wollastonite reaction rims. This model reproduces many of the measured ¦Äp xmlns="""">18p>O values of wollastonite reaction rims of the current study to within ¡À 1? even though the wollastonite compositions vary by almost 10?