在苏亚雷斯的Puesto suarez火山综合体的K-Ar水时代,里约热内卢Negro

Q3 Agricultural and Biological Sciences
M. Remesal, F. Salani
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引用次数: 1

摘要

Agua de la Piedra火山复合体(APVC)被定义为Quinelaf超单元的一个组成部分,其中包括比所谓的Somun Cura玄武岩高原更年轻的双峰序列。高原和后高原积液对应于苏蒙库拉岩浆省(SCMP)的主要时期。APVC出现在高原西缘,由玄武岩至粗灰质的熔岩和火山碎屑岩组合而成。层序出露范围内的岩心主要为中硅质,基底流呈放射状分布。在粗纤维部位的东端,可以辨认出至少有两个粗纤维变种的圆顶状体。颗粒状岩石的K-Ar年龄证实了奎尼莱夫超单元中存在不止一次的涌出事件,并建立了一些标准来讨论其与玄武岩高原的关系。©2018阿根廷自然科学博物馆贝纳迪诺里瓦达维亚。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
K-Ar Age of Agua de la Piedra Volcanic Complex at Puesto Suárez, Río Negro
The Agua de la Piedra Volcanic Complex (APVC) has been defined as an integral part of the Quinelaf Superunit, which includes younger bimodal sequences than the so-called basaltic plateau of Somun Cura. The plateau and post-plateau effusions correspond to the major episodes of the Somun Cura Magmatic Province of (SCMP). The APVC emerges in the western periphery of the plateau and is composed of an association of lavas and pyroclastites from basaltic to trachytic. The core of the range on which the sequence crops out is mainly mesosilicic and the basic flows of radially disposed. At the eastern end of the trachyte site a dome-shaped body with at least two trachytic varieties is recognized. The K-Ar age of the grainy variety allows corroborating the presence of more than one effusive event within the Quinelaf Superunit and establishing some criteria to discuss its relationship with the basaltic plateau. © 2018 Museo Argentino de Ciencias Naturales Bernardino Rivadavia.
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来源期刊
Revista del Museo Argentino de Ciencias Naturales, Nueva Serie
Revista del Museo Argentino de Ciencias Naturales, Nueva Serie Agricultural and Biological Sciences-Animal Science and Zoology
CiteScore
1.00
自引率
0.00%
发文量
7
审稿时长
12 weeks
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