دورية أكاديمية

Interaction of magma with sedimentary wall rock and magnetite ore genesis in the Panzhihua mafic intrusion, SW China

التفاصيل البيبلوغرافية
العنوان: Interaction of magma with sedimentary wall rock and magnetite ore genesis in the Panzhihua mafic intrusion, SW China
المؤلفون: Ganino, Clément, Arndt, Nicholas, Zhou, Mei-Fu, Gaillard, Fabrice, Chauvel, Catherine
المساهمون: Laboratoire de Géodynamique des Chaines Alpines (LGCA), Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS), Géoazur (GEOAZUR 6526), Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Université Nice Sophia Antipolis (1965 - 2019) (UNS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur, Université Côte d'Azur (UniCA)-Université Côte d'Azur (UniCA)-Centre National de la Recherche Scientifique (CNRS), Department of Earth Sciences Hong kong, The University of Hong Kong (HKU), Institut des Sciences de la Terre d'Orléans (ISTO), Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Université de Tours (UT)-Centre National de la Recherche Scientifique (CNRS), LGCA, ISTO, Hong Kong University
المصدر: ISSN: 0026-4598 ; Mineralium Deposita ; https://hal.science/hal-00352271Test ; Mineralium Deposita, 2008, 43, pp.677-694. ⟨10.1007/s00126-008-0191-5⟩.
بيانات النشر: HAL CCSD
Spinger
سنة النشر: 2008
المجموعة: HAL Université Côte d'Azur
مصطلحات موضوعية: magma, sediment, magnetite ore, oxygen fugacity, skarn, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences
الوصف: International audience ; In SW China, several large magmatic Fe-Ti-V oxide ore deposits are hosted by gabbroic intrusions associated with the Emeishan flood basalts. The Panzhihua gabbroic intrusion, a little deformed sill that contains a large titanomagnetite deposit at its base, concordantly intrudes late- Proterozoic dolostones. Mineralogical and chemical studies of the contact aureole in the footwall dolostones demonstrates that the metamorphism was largely isochemical, but for the release of large quantities of CO2 as the rocks were converted to marble and skarns during intrusion of the gabbroic magma. Petrological modelling of the crystallization of the intrusion, using H2O-poor Emeishan basalt as parent magma, shows that under normal conditions Fe-Ti-oxides crystallize at a late stage, after the crystallization of abundant olivine, clinopyroxene and plagioclase. In order for titanomagnetite to separate efficiently to form the ore deposit, this mineral must have crystallized earlier and close to the liquidus. We propose that CO2-rich fluids released during decarbonatization of sedimentary floor rocks passed up through the magma. Redox equilibria calculations show that when magma with the composition of Emeishan basalt is fluxed by a CO2-rich gas phase, its equilibrium oxygen fugacity (fO2) increases from FMQ to FMQ+1.5. From experimental constraints on magnetite saturation in basaltic magma under controlled fO2, such an oxidizing event would allow magnetite to crystallize near to the liquidus, leading to the formation of the deposit.
نوع الوثيقة: article in journal/newspaper
اللغة: English
العلاقة: hal-00352271; https://hal.science/hal-00352271Test; https://hal.science/hal-00352271/documentTest; https://hal.science/hal-00352271/file/GaninoMinDep.pdfTest
DOI: 10.1007/s00126-008-0191-5
الإتاحة: https://doi.org/10.1007/s00126-008-0191-5Test
https://hal.science/hal-00352271Test
https://hal.science/hal-00352271/documentTest
https://hal.science/hal-00352271/file/GaninoMinDep.pdfTest
حقوق: info:eu-repo/semantics/OpenAccess
رقم الانضمام: edsbas.95986651
قاعدة البيانات: BASE