A Cautionary Note on Amphibole Geobarometry

J. Molina, A. Cambeses, J. Moreno, I. Morales, C. Lázaro, P. Montero, F. Bea
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引用次数: 1

Abstract

The classical Al-in-hornblende barometer has been very successful in determining the depth of intrusion of metaluminous cordilleran granitoid plutons that bear the buffering assemblage at near solidus conditions: hornblende-biotite-plagioclase-orthoclase-quartz-sphene-two Fe-Ti-oxides (or one Fe-Ti oxide + epidote)-melt-vapor (e.g., [1-3]). Ridolfi et al. [4] and Ridolfi and Renzulli [5] derived empirical amphibole-only barometric expressions that could be potentially applied to a larger number of phenocrystic assemblages from volcanic rocks. However, Erdmann et al. [6] claimed that these barometers are inaccurate and can give untenable estimates. A graphical barometer based on the partitioning of Al and Si between amphibole and plagioclase was derived by Fershtater [7] using amphibole-plagioclase compositional pairs of rocks from the Urals. More recently, Molina et al. [8] calibrated an empirical expression based on experimental data that can be applied to igneous and high-grade metamorphic rocks. In order to compare the reliability of amphibole-only and amphibole-plagioclase barometry, in this work, we test the performance of the expressions of Ridolfi and Renzulli [5] and Molina et al. [8], using an experimental data set compiled from the literature that has been recently published by Molina et al. [9]. In accordance with Erdmann et al.[6], the test reveals unsustainable pressure estimates with the amphibole-only barometric expressions from Ridolfi and Renzulli [5]. By contrast, the amphibole-plagioclase barometer from Molina et al. [8] performs well and yields a precision better than 1.7 kbar for Qz-Amp-Pl and Ol-free-Cpx-Amp-Pl assemblages with amphibole compositions having > 1 apfu (23O; normalisation to 13-CNK) Al, 0.05-0.27 apfu Ti: and < 1.07 apfu Fe3+. References 1. Hammarstrom and Zen, 1986, American Mineralogist 71, 1297–1313. 2 Schmidt, 1992, Contributions to Mineralogy and Petrology 110, 304–310. 3. Anderson and Smith, 1995, American Mineralogist 80, 549-449. 4. Ridolfi et al., 2010, Contributions to Mineralogy and Petrology 160, 45–66. 5. Ridolfi and Renzulli, 2012, Contributions to Mineralogy and Petrology 163, 877–895. 6. Erdmann et al., 2014, Contributions to Mineralogy and Petrology 167, 1016 7. Fershtater, 1990, Geokhimiya 3, 328–335. 8. Molina et al., 2015, Lithos 232 286–305. 9. Molina et al., 2020; American Mineralogist, in press, https://doi.org/10.2138/am-2020-7400
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关于角闪洞地理测量的警告
经典的al -in-角闪石气压计非常成功地确定了在近固相条件下具有缓冲组合的铝质科迪勒岩花岗岩类岩体的侵入深度:角闪石-黑云母-斜长石-正长石-石英-榍石-两种铁-钛氧化物(或一种铁-钛氧化物+绿帘石)-熔融蒸汽(例如[1-3])。Ridolfi et al.[4]和Ridolfi and Renzulli[5]推导出仅角闪岩的经验气压表达式,这些表达式可能应用于更多的火山岩斑晶组合。然而,Erdmann等人声称,这些晴雨表是不准确的,可以给出站不住脚的估计。Fershtater b[7]利用乌拉尔地区的角闪石-斜长石组成对,导出了一个基于角闪石-斜长石之间Al和Si分异的图解晴雨表。最近,Molina等人根据实验数据校准了一个经验表达式,该表达式可应用于火成岩和高级变质岩。为了比较双角石-斜长石和双角石-斜长石气压测定法的可靠性,在这项工作中,我们使用Molina et al.[9]最近发表的文献中编译的实验数据集,测试了Ridolfi和Renzulli[5]和Molina et al.[8]的表达式的性能。根据Erdmann等人[bb1]的研究,该测试揭示了Ridolfi和Renzulli bb1仅含角闪石的气压表达式的不可持续压力估计。相比之下,Molina et al.[8]的角闪石-斜长石气压计表现良好,对于含有> 1 apfu (23O)的角闪石成分的Qz-Amp-Pl和Ol-free-Cpx-Amp-Pl组合,精度优于1.7 kbar;正态化到13-CNK) Al, 0.05-0.27 apfu Ti:和< 1.07 apfu Fe3+。引用1。陈志刚,1986,《矿物学》第1期,1297-1313页。[2]施密特,1992,矿物学与岩石学的贡献(11),304-310。3.安德森和史密斯,1995,美国矿物学80,549-449。4. Ridolfi et al., 2010,矿物学与岩石学贡献,160,45-66。5. Ridolfi和Renzulli, 2012,矿物学和岩石学贡献163,877-895。6. Erdmann et al., 2014,矿物学和岩石学贡献167,1016。科学通报,1990,3(3):328-335。8. Molina et al., 2015, vol . 32(2): 286-305。9. Molina et al., 2020;美国矿物学家,出版中,https://doi.org/10.2138/am-2020-7400
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