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首页> 外文期刊>Quaternary geochronology >Composition, pre-eruptive zonation, and geochronologic significance of the ~450ka Diamante Tuff, Andean Cordillera (34°S), Argentina
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Composition, pre-eruptive zonation, and geochronologic significance of the ~450ka Diamante Tuff, Andean Cordillera (34°S), Argentina

机译:阿根廷安第斯山脉(34°S)〜450ka​​ Diamante Tuff的组成,火山爆发前的带化及其地质年代学意义

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摘要

Vertical geochemical sampling through the Diamante Tuff establishes patterns of zonation in the pre-eruption magma. Volcanic glass demonstrates a roofward increase in Fe and Cl, and a roofward decrease in Ca. Trace elements have no measurable zonation. Welded volcanic glass shows post-eruption loss of Fe, Mg and Cl as well as K gain. Our reported glass chemistry provides robust criteria for correlation to other localities. The Diamante Tuff is an important stratigraphic marker and recognition of this unit provides age control on Quaternary deposits, allowing determination of process rates and elucidating timing of tectonic and geomorphic activity.
机译:通过Diamante Tuff进行的垂直地球化学采样在喷发前的岩浆中建立了分区模式。火山玻璃显示出Fe和Cl的向屋顶增加,而Ca的向屋顶减少。痕量元素没有可测量的分区。焊接的火山玻璃显示出喷发后铁,镁和氯的损失以及钾的增加。我们报告的玻璃化学性质提供了与其他地区相关的可靠标准。 Diamante Tuff是重要的地层标记,该单元的识别提供了第四纪沉积物的年龄控制,从而可以确定过程速率并阐明构造和地貌活动的时间。

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