2009
DOI: 10.1016/j.chemgeo.2009.03.013
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Boron isotope composition of tourmalinite and vein tourmalines associated with gold mineralization, Serra do Itaberaba Group, central Ribeira Belt, SE Brazil

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Cited by 38 publications
(17 citation statements)
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“…It is for these reasons that the use of stable B-isotopes in tourmaline has become well established in the study of ore deposits (e.g. Palmer and Slack, 1989;Xavier et al, 2008;Garda et al, 2009;Slack and Trumbull, 2011;Tornos et al, 2012;Duncan et al, 2014;Molnár et al, 2016). While boron isotope analysis by thermal ionization mass spectrometry (TIMS) requires complete chemical dissolution of a bulk tourmaline sample, secondary ion mass spectrometry (SIMS) allows for texturally resolved measurement of δ 11 B in tourmaline at levels of precision that allow detailed analysis of fluid source reservoirs in relation to the mineral paragenesis.…”
Section: Introductionmentioning
confidence: 99%
“…It is for these reasons that the use of stable B-isotopes in tourmaline has become well established in the study of ore deposits (e.g. Palmer and Slack, 1989;Xavier et al, 2008;Garda et al, 2009;Slack and Trumbull, 2011;Tornos et al, 2012;Duncan et al, 2014;Molnár et al, 2016). While boron isotope analysis by thermal ionization mass spectrometry (TIMS) requires complete chemical dissolution of a bulk tourmaline sample, secondary ion mass spectrometry (SIMS) allows for texturally resolved measurement of δ 11 B in tourmaline at levels of precision that allow detailed analysis of fluid source reservoirs in relation to the mineral paragenesis.…”
Section: Introductionmentioning
confidence: 99%
“…It is thus unlikely that there was a substantial fractionation of sodalite during the formation of the Nb-Ta-mineralized and Nb-Ta-poor syenitic dikes. The Nb-Ta-mineralized and Nb-Ta-poor syenitic dikes and syenitic plutons in the Panxi region have δ 11 B values similar to those of terrestrial sediments, far below the value of seawater and/or fluid (Garda et al, 2009) (Fig. 10b).…”
Section: A Transition From Magmatic To Hydrothermal Stagementioning
confidence: 88%
“…Exhalative activity was responsible for the genesis of both tourmaline-bearing rocks and iron mineralisation. When metamorphosed, these protoliths produced tourmalinites and the metamorphic product of Algoma-type iron formation, both enriched with syngenetic gold mineralisation (Juliani 1993;Garda et al 2003Garda et al , 2005Garda et al , 2009Beljavskis et al 2003Beljavskis et al , 2005. Within this group, lowangle epigenetic shear zone-related gold mineralisation also occurs due to remobilisations of syngenetic gold (Martin et al 1998).…”
Section: Precambrian Metallic Mineralisationsmentioning
confidence: 99%