黄金科学技术 ›› 2022, Vol. 30 ›› Issue (6): 848-865.doi: 10.11872/j.issn.1005-2518.2022.06.074
• 矿产勘查与资源评价 • 上一篇
王华1(),邹少浩1(),陈龙2,许德如1,陈喜连1,王雪娜1,冯浩东1
Hua WANG1(),Shaohao ZOU1(),Long CHEN2,Deru XU1,Xilian CHEN1,Xuena WANG1,Haodong FENG1
摘要:
赣西地区浒坑钨矿是我国华南钨、锡、铜多金属成矿区与中生代岩浆活动密切相关的典型矿床之一。对浒坑钨矿床中与成矿有关的白云母花岗岩开展了锆石U-Pb定年、磷灰石和锆石原位微量元素研究,结果表明:赋矿白云母花岗岩的成岩时代为(152.3±1.73)Ma;磷灰石具有特殊的“M”型REE球粒陨石标准化配分模式,富F和Mn,贫Cl和Mg;锆石具有高Th/U比值,REE球粒陨石标准化配分模式亏损LREE、富集HREE。锆石微量元素(Ce、U和Ti)温度计和氧逸度计结果表明,锆石形成于岩浆早期高温(800 ℃)和低氧逸度条件下。研究认为,浒坑赋矿花岗岩在演化初期经历了强烈的矿物结晶分异,矿床的形成可能与还原性高分异岩浆演化相关。
中图分类号:
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