Reply to Muntener and Baumgartner comment on: 'Spatially controlled Fe and Si isotope variations: an alternative view on the formation of the Torres del Paine pluton'

Gajos Norbert A.; Lundstrom Craig L.; Taylor Alexander H.; Drinkall Dana E.

首页> 外文期刊>Contributions to Mineralogy and Petrology >Reply to Muntener and Baumgartner comment on: 'Spatially controlled Fe and Si isotope variations: an alternative view on the formation of the Torres del Paine pluton'

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Reply to Muntener and Baumgartner comment on: 'Spatially controlled Fe and Si isotope variations: an alternative view on the formation of the Torres del Paine pluton'

机译：回复Muntener和Baumgartner评论：“空间控制的Fe和Si同位素变异：托雷斯德尔潘恩普鲁顿的形成替代视图

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Muntener and Baumgartner (Contrib Mineral Petrol, 2019) comment on our interpretations of the petrogenetic processes operating within the Torres del Paine Intrusive complex (Gajos et al., in Contrib Mineral Petrol 171(11):93, 2016). The issues raised reflect either points that are subject to interpretation or misrepresentations of the data we provided. We dispute field observations and counter that their model reflects over-interpretation due to limited age dating. We provide new geothermometry data indicating that marginal granites formed in a cold environment, consistent with our original model. The Fe and Sr data are not consistent with their two endmember mixing argument. We conclude by reaffirming our position that the thermal migration zone refining process provides a viable explanation for the isotopic variation and construction of the Torres del Paine pluton.

机译：Muntener和Baumgartner（Concormileral Petrol，2019）就我们对托雷斯德尔潘恩侵入性复合物（Gajos等，Gajos等人，Concormilal Petrol 171（11）：93,2016）的解释评论。提出的问题反映了有关我们提供的数据的解释或歪曲的要点。由于年龄约会有限，我们争取现场观察和反击其模型反映过度解释。我们提供新的地热测定数据，表明在寒冷环境中形成的边缘花岗岩，与我们原来的模型一致。 FE和SR数据与他们的两个终点混合论证不一致。我们通过重申我们的地位，即热迁移区炼油过程为同位素变异和托雷斯德尔潘恩芦苇的建设提供了可行的解释。

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来源
《Contributions to Mineralogy and Petrology》 |2019年第6期|共6页
作者
Gajos Norbert A.; Lundstrom Craig L.; Taylor Alexander H.; Drinkall Dana E.;
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作者单位

Univ Illinois Dept Geol Champaign IL 61820 USA;

Univ Illinois Dept Geol Champaign IL 61820 USA;

Univ Illinois Dept Geol Champaign IL 61820 USA;

Univ Illinois Dept Geol Champaign IL 61820 USA;

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原文格式 PDF
正文语种 eng
中图分类矿物学;岩石学;
关键词
Torres del Paine; Magma chamber; Magma differentiation; Fe isotopes; Si isotopes; Thermal diffusion;

机译：Torres del Paine;岩浆室;岩浆分化;Fe同位素;Si同位素;热扩散;

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1. Reply to Muntener and Baumgartner comment on: "Spatially controlled Fe and Si isotope variations: an alternative view on the formation of the Torres del Paine pluton' [J] . Gajos Norbert A., Lundstrom Craig L., Taylor Alexander H., Contributions to Mineralogy and Petrology . 2019,第6期

机译：回复Muntener和Baumgartner评论：“空间控制的Fe和Si同位素变异：托雷斯德尔潘恩普鲁顿的形成替代视图
2. Comment on: "Spatially controlled Fe and Si isotope variations: an alternative view on the formation of the Torres del Paine pluton' by Gajos et al. (Contrib Mineral Petrol 171:93, 2016) [J] . Muentener Othmar, Baumgartner Lukas Contributions to Mineralogy and Petrology . 2019,第6期

机译：评论：“空间控制的FE和SI同位素变化：GAJOS等人的形成托雷斯德尔潘恩普鲁顿的替代视图。（挑剔矿物汽油171：93,2016）
3. Spatially controlled Fe and Si isotope variations: an alternative view on the formation of the Torres del Paine pluton [J] . Gajos Norbert A., Lundstrom Craig C., Taylor Alexander H. Contributions to Mineralogy and Petrology . 2016,第11期

机译：空间控制的Fe和Si同位素变化：关于Torres del Paine岩体形成的另一种观点
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5. Source and fractionation controls on subduction-related plutons and dike swarms in southern Patagonia (Torres del Paine area) and the low Nb/Ta of upper crustal igneous rocks [O] . Othmar Müntener, Tanya Ewing, Lukas P. Baumgartner, -1

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Reply to Muntener and Baumgartner comment on: 'Spatially controlled Fe and Si isotope variations: an alternative view on the formation of the Torres del Paine pluton'

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