岩矿测试2025，Vol.44Issue(1)：88-101,14.DOI:10.15898/j.ykcs.202404030074
柳江盆地髫髻山组凝灰岩地球化学与熔体包裹体水含量特征
Geochemical Characteristics and Water Content of Melt Inclusions in the Tuff of the Tiaojishan Formation,Liujiang Basin
摘要
Abstract
Water,as the primary volatile component in magmatic systems,has a significant impact on the formation and evolution of magma.The Tiaojishan Formation igneous rocks in the Liujiang Basin are significant products of Yanshanian volcanic activity.Although previous studies have extensively explored their geochemical characteristics,the water content of the magma in the Liujiang Basin during Yanshanian volcanic activity remains unclear.Melt inclusions,which capture the original magmatic information,serve as the most direct samples for determining the water content of magma.Based on geochemical analysis,this study quantitatively determines the water content in melt inclusions using laser Raman spectroscopy with standard samples.The results show that the lower tuff samples of the Tiaojishan Formation are characterized by high Si and Al contents,enrichment in LILEs,depletion in HFSEs,enrichment in LREEs,and depletion in HREEs.The water content in melt inclusions reveals a range of 0.99%to 4.98%,with an average of 2.62%.These characteristics jointly indicate the water-enriched acidic magmatic activity during the early Tiaojishan period in this area.Combining the water content of melt inclusions with the large-scale volcanic eruptions in the stage,this study suggests that high water content in the magma enhanced the eruptive dynamics of the magmatic system,making it a contributing factor to the large-scale volcanic eruption.The BRIEF REPORT is available for this paper at http://www.ykcs.ac.cn/en/article/doi/10.15898/j.ykcs.202404030074.关键词
柳江盆地/髫髻山组/凝灰岩/熔体包裹体/水含量/显微激光拉曼光谱法Key words
Liujiang Basin/Tiaojishan Formation/tuff/melt inclusions/water content/laser Raman spectroscopy分类
地质学引用本文复制引用
赵汇珍,陈勇,涂聪,冯艳伟..柳江盆地髫髻山组凝灰岩地球化学与熔体包裹体水含量特征[J].岩矿测试,2025,44(1):88-101,14.基金项目
国家自然科学基金项目(41873070,42173042) （41873070,42173042）
