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<identifier>oai:HAL:hal-01260258v1</identifier>
<datestamp>2018-01-11</datestamp>
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<publisher>HAL CCSD</publisher>
<title lang=en>Chemical mass transfer in shear zones and metacarbonate xenoliths: a comparison of four mass balance approaches</title>
<creator>Durand, Cyril</creator>
<creator>Oliot, Emilien</creator>
<creator>Marquer, Didier</creator>
<creator>Sizun, Jean Pierre</creator>
<contributor>Laboratoire de Génie Civil et Géo-Environnement (LGCgE) ; Université de Lille, Sciences et Technologies</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Dylbas ; Institut de physique du globe de Strasbourg (IPGS) ; Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Laboratoire Chrono-environnement (LCE) ; Université Bourgogne Franche-Comté (UBFC) - Centre National de la Recherche Scientifique (CNRS) - Université de Franche-Comté (UFC)</contributor>
<description>International audience</description>
<source>ISSN: 0935-1221</source>
<source>European Journal of Mineralogy</source>
<publisher>E Schweizerbart Science Publishers</publisher>
<identifier>hal-01260258</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01260258</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01260258</source>
<source>European Journal of Mineralogy, E Schweizerbart Science Publishers, 2015, 27 (6), pp.731-754. 〈http://eurjmin.geoscienceworld.org/content/27/6/731.abstract?sid=a1ed2163-652d-46b5-b632-01b7f29d2b9e〉. 〈10.1127/ejm/2015/0027-2475〉</source>
<identifier>DOI : 10.1127/ejm/2015/0027-2475</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1127/ejm/2015/0027-2475</relation>
<source>http://eurjmin.geoscienceworld.org/content/27/6/731.abstract?sid=a1ed2163-652d-46b5-b632-01b7f29d2b9e</source>
<language>en</language>
<subject lang=fr> exoskarn</subject>
<subject lang=fr> Aar Massif</subject>
<subject lang=fr> Quérigut Massif</subject>
<subject lang=fr>chemical mass transfer</subject>
<subject lang=fr> mass balance calculation</subject>
<subject lang=fr> metasomatism</subject>
<subject lang=fr> ductile shear zone</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<subject>[SDU.STU.PE] Sciences of the Universe [physics]/Earth Sciences/Petrography</subject>
<subject>[SDU.STU.MI] Sciences of the Universe [physics]/Earth Sciences/Mineralogy</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>Mass balance calculations have been performed through a comparison of published graphical and statistical approaches applied to two contrasted geological settings: (i) the development of a greenschist-facies ductile shear-zone that recorded a weak volume change but significant mass transfers, and (ii) the formation of exoskarns in metacarbonate xenoliths that recorded a large volume decrease related to huge mass transfers. The comparison of the four mass-balance approaches shows that, if uncertainties are ignored, (1) they yield similar results concerning the mobile vs immobile behaviour of many components; (2) they yield similar mass-change values on bulk rock and on individual chemical elements (bulk-rock mass-change values differ by a maximum of ca. 15 % between graphical and statistical treatments of the metacarbonate xenolith evolution). The main difference concerns the uncertainties on mass changes (for bulk rocks and individual elements), which are much larger with the graphical than with the statistical approaches when uncertainties on chemical elements are taken into account, as they should be.The main advantage of the graphical methods is their rapid implementation and the clarity of the diagrams. Their main disadvantages are that uncertainties on each chemical element and bulk compositions are not taken into account and the difficulty in choosing an accurate immobility field to precisely define errors. Graphical methods need to be completed by a statistical treatment that gives absolute mass transfer results. The statistical approaches have the advantage of taking into account the chemical heterogeneities of the compared populations, in conjunction to a precise data treatment. The statistical treatment is an important and necessary step to decipher and to be pertinent in interpreting mobility/immobility of chemical elements, and, thus, in the absolute quantification of mass and volume changes.</description>
<date>2015-12</date>
</dc>
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