基于XRF地球化学分析的北哥伦塔洛地区安山岩成因研究

Fandji Marfian, A. P. Permana, N. Akase
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引用次数: 2

摘要

研究区域为北哥伦塔洛县Kwandang区Bualemo村。坐标为北纬0˚47′10”~ 0˚48′40”,东经122˚55′0”~ 122˚57′5”,面积约10 km2。本研究旨在确定研究区安山岩的成因和构造背景。本研究采用填图法确定研究地点的地质条件,x射线荧光(XRF)地球化学分析确定岩石的化学成分。结果表明,研究区地层从最古老到最年轻依次为安山岩单元、蚀变安山岩单元和冲积沉积单元。研究区地质构造为一个大致方向为相对南北的张节理。张力节理结构数据分析结果为n171oe /79o。根据地球化学结果,发现岩浆类型为拉斑岩,其名称为玄武岩和玄武岩粗面安山岩。岩浆来源为岛弧拉斑岩和岛弧钙碱性玄武岩,研究区构造背景为两洋俯冲,即苏拉威西海板块与苏拉板块之间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study of Petrogenesis Andesite Rock in Bualemo Region, North Gorontalo Regency Based on XRF Geochemistry Analysis
The research area is Bualemo Village, Kwandang District, North Gorontalo Regency. With coordinates 0˚ 47' 10" - 0˚ 48' 40" North Latitude and 122˚ 55' 0" - 122˚ 57' 5" East Longitude with an area of about 10 km2. This study aims to determine the petrogenesis of andesite rocks and the tectonic setting in the study area. The method used in this study is a mapping method to determine the geological conditions of the research site and X-ray fluorescence (XRF) geochemical analysis to determine the chemical content of rocks. The results showed that the stratigraphy of the study area, sorted from oldest to youngest, was an andesite unit, an altered andesite unit, and an alluvial deposit unit. The geological structure in the study area is a tension joint with a general direction of relative north-south. The tension joint structure data analysis results have a value of N 171oE/79o. Based on geochemistry results, it was found that the type of magma is tholeiitic, with its name basalt and basaltic trachyte andesite. The origin of the magma is island arc tholeiitic and island arc calc-alkaline basalt, with the tectonic setting of the study area being subduction between two oceans, namely between the Sulawesi sea plate and the Sula plate.
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