吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (2): 455-472.doi: 10.13278/j.cnki.jjuese.20200009
• 地质与资源 • 上一篇
邹国庆1, 余牛奔1, 孙国庆1, 黄修保2, 尼加提·阿布都逊3,4, 卢观送1
Zou Guoqing1, Yu Niuben1, Sun Guoqing1, Huang Xiubao2, Nijiati·Abuduxun3,4, Lu Guansong1
摘要: 本文对东准噶尔造山带三塘湖盆地西北缘奥依托浪格地区石炭纪巴塔玛依内山组进行了火山岩地质、岩相学、地球化学特征研究,并结合相关年代学成果,探讨了火山岩成因、形成环境与东准噶尔造山带构造演化。研究认为:该区石炭纪巴塔玛依内山组火山岩具明显的陆相火山岩、双峰式火山岩特征,岩石组合基性端元以玄武岩为主,酸性端元为珍珠岩、英安岩;主量元素特征显示基性端元为钙碱—碱性性质,酸性端元珍珠岩、英安岩分别属于碱性、拉斑性质;微量元素特征显示基性端元相对富集Ba、K、Sr等大离子亲石元素(LILE),亏损Th、Nb、Nd等高场强元素(HFSE),酸性端元强烈亏损Ba、Nb、Sr、Sm、Ti等元素,富集K元素;稀土元素显示两端元均为轻稀土元素(LREE)相对富集、重稀土元素(HREE)相对亏损特征;珍珠岩主、微量元素特征与整体具有明显差异。综合研究表明:该双峰式火山岩基性端元来源于地幔岩的部分熔融,酸性端元英安岩来源于基性端元的分离结晶作用,珍珠岩则来源于下地壳的部分熔融;地球动力学背景为俯冲洋壳的拆沉作用,造成软流圈热源上涌,引发地幔岩的部分熔融与岩石圈的伸展减薄,进而诱发下地壳镁铁质岩的减压熔融;构造环境为后碰撞伸展阶段晚期,并指示了板块链式缝合的特点。
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