<?xml version="1.1" encoding="utf-8"?>
<article xsi:noNamespaceSchemaLocation="http://jats.nlm.nih.gov/publishing/1.1/xsd/JATS-journalpublishing1-mathml3.xsd" dtd-version="1.1" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"><front><journal-meta><journal-id journal-id-type="publisher-id">ADA</journal-id><journal-title-group><journal-title>Architectural Design and Application</journal-title></journal-title-group><issn>2995-3219</issn><eissn>2992-9857</eissn><publisher><publisher-name>Art and Technology</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.61369/ADA.2026010066</article-id><article-categories><subj-group subj-group-type="heading"><subject>Article</subject></subj-group></article-categories><title>钨锡矿化花岗岩地球化学分异规律</title><url>https://artdesignp.com/journal/ADA/4/1/10.61369/ADA.2026010066</url><author>徐鹏,鲁新丽,张克亮</author><pub-date pub-type="publication-year"><year>2026</year></pub-date><volume>4</volume><issue>1</issue><history><date date-type="pub"><published-time>2026-06-20</published-time></date></history><abstract>钨锡矿化花岗岩演化中呈现显著的地球化学分异，分异方向与程度直接影响矿质的聚集与释放，岩浆上升冷凝过程中持续分离亲石元素与亲流体元素，使富挥发分熔体具备运移金属的能力，多阶段分异让示踪元素分布趋向高演化端元，形成利于钨锡富集的弱还原环境。随温压条件改变，金属与挥发分由深部向浅部运移，在构造薄弱带形成局部富集，花岗质岩浆体系内微量元素分布、挥发分富集及残余组分演变，共同控制钨锡矿化的时序与规模，这一分异规律揭示矿化花岗岩内部物质传输路径，可为判断岩浆成矿潜力提供依据。</abstract><keywords>钨锡矿化, 花岗岩, 地球化学分异, 挥发分富集, 岩浆演化</keywords></article-meta></front><body/><back><ref-list><ref id="B1" content-type="article"><label>1</label><element-citation publication-type="journal"><p>[1]LI W ,TANG J ,GUO N , et al. Robust Timing Constraints for Granitic Magmatism and Hydrothermal Mineralization in the Tieshanlong W ‐Sn Ore Field, Eastern Nanling Range, South China [J]. Acta Geologica Sinica ‐ English Edition, 2024, 98 (5): 1255-1269. DOI:10.1111/1755-6724.15212.
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