M. Remesal, M. E. Cerredo, P. Cordenons, J. Albite
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引用次数: 2
摘要
这篇文章涉及位于安第斯山脉北部巴塔哥尼亚的索蒙库拉岩浆省内的科罗娜奇科火山。研究区域位于Alta Sierra de Somun Cura火山复合体的北部,由几个不同形态的玄武岩火山建筑组成:喷溅锥,凝灰岩环和与小型盾状火山(胸骨型)相关的长熔岩流。岩石学特征和全岩化学成分表明,碱含量呈时间递进式增加,晚期由早期过渡期向玄武质过渡。模拟结果表明,Las Lomadas岩石为石榴石-尖晶石相的小行星圈源,其部分熔融百分比较低(< 7-8%)。在研究的岩石组中,飞溅锥序列与Alta Sierra de Somun Cura火山杂岩的玄武岩组分具有地球化学亲和性。
The volcanic association of Las Lomadas area, Corona Chico Volcanites. Somún Curá Magmatism. Río Negro province, Argentina
This contribution deals with the Corona Chico Vulcanites, within the Somun Cura Magmatic Province, northern Extra-Andean Patagonia. The studied area is located to the north of the Alta Sierra de Somun Cura Volcanic Complex and is made of several basaltic volcanic buildings of varied morphologies: spatter cones, tuff ring and long lava flows related to small shield volcanoes (of scutulum type). Petrographic characteristics as well as whole rock chemical composition suggest a time progressive increase in alkalis content and a shift from early transitional terms to basanitic rocks in the latest stages. A simulation of the source yielded for Las Lomadas rocks an astenospheric source in the garnet-spinel facies, with associated low partial melting percentages (< 7-8%). Within the studied rock set, the spatter cones sequence displays geochemical affinities with the basaltic component of Alta Sierra de Somun Cura Volcanic Complex.