Study of Element Abundance in Volcanic Rocks in the Beruang Kanan Region, Gunung Mas Regency, Central Kalimantan

Retno Anjarwati, S. Sutarto, D. Yudiantoro, A. Idrus
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Abstract

Soil elements, based on their abundance in the earth's crust and petrogenetic analysis aim to divide soil elements into several groups, namely major elements, trace elements and rare earth elements (REE). The research location is located in the Beruang Kanan area, Tumbang Miri District, Gunung Mas Regency, Central Kalimantan Province. The major elements and trace elements of the host rock were obtained from X-ray fluorescence (XRF) analysis and Plasma-Coupled Mass Spectrometry (ICP-MS) methods. Volcanic rocks from the Kanan Bear prospect The volcanic magmatic affinity in the study area is calc-alkaline this chemical characteristic is clearly reflected by the type of volcanic rock which is determined based on its chemical classification, which is generally igneous rock of the calc-alkaline magma series type so it is interpreted to originate from a convergent tectonic environment continental edge.
中加里曼丹古贡马斯地区 Beruang Kanan 地区火山岩元素丰度研究
根据土壤元素在地壳中的丰度和岩石成因分析,旨在将土壤元素分为几组,即主要元素、微量元素和稀土元素(REE)。研究地点位于中加里曼丹省 Gunung Mas 县 Tumbang Miri 区 Beruang Kanan 地区。通过 X 射线荧光(XRF)分析和等离子体耦合质谱(ICP-MS)方法获得了主岩的主要元素和微量元素。卡南熊探矿区的火山岩 研究区的火山岩浆亲和性为钙碱性,这一化学特征明显反映在火山岩的类型上,而火山岩的类型是根据其化学分类确定的,一般为钙碱性岩浆系列类型的火成岩,因此可以解释为源自汇聚构造环境的大陆边缘。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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