周口店官地杂岩中斜长角闪岩的年代学、地球化学及其地质意义

苑东洋, 李德威, 陈棋, 曾平, 徐其虎. 周口店官地杂岩中斜长角闪岩的年代学、地球化学及其地质意义[J]. 西北地质, 2016, 49(2): 149-164.
引用本文: 苑东洋, 李德威, 陈棋, 曾平, 徐其虎. 周口店官地杂岩中斜长角闪岩的年代学、地球化学及其地质意义[J]. 西北地质, 2016, 49(2): 149-164.
YUAN Dongyang, LI Dewei, CHEN Qi, ZENG Ping, XU Qihu. Geochronology and Geochemical Characteristics of Amphibolite in Guandi Complex, Zhoukoudian Area and Its Geological Significance[J]. Northwestern Geology, 2016, 49(2): 149-164.
Citation: YUAN Dongyang, LI Dewei, CHEN Qi, ZENG Ping, XU Qihu. Geochronology and Geochemical Characteristics of Amphibolite in Guandi Complex, Zhoukoudian Area and Its Geological Significance[J]. Northwestern Geology, 2016, 49(2): 149-164.

周口店官地杂岩中斜长角闪岩的年代学、地球化学及其地质意义

  • 基金项目: 中国地质调查局"云南1:5万龙朋等六幅区域地质调查"(1212011220400)

Geochronology and Geochemical Characteristics of Amphibolite in Guandi Complex, Zhoukoudian Area and Its Geological Significance

  • 周口店房山岩体南北两侧的官地杂岩主要由长英质片麻岩、斜长角闪岩和混合岩组成。笔者首次对东岭子官地杂岩中斜长角闪岩进行研究,斜长角闪岩LA-ICP-MS锆石U-Pb测年上交点年龄为(2 551±37)Ma,代表岩浆结晶年龄。其地球化学显示具有低TiO2,高MgO的特点,Mg#平均值为70, LREE与HREE分异度高,具有Eu的负异常。地球化学特征和岩相学揭示其岩浆经历分离结晶作用,原岩矿物主要由辉石、斜长石组成。锆石Hf同位素εHf(t)处于亏损地幔演化线和球粒陨石之间示踪源区为岩石圈富集地幔,微量元素方面富集LILE(Rb, Ba, K),亏损HFSE(Nb, Ta, Zr)的特点显示岛弧有关的富集地幔源区。初步认为大洋板片向东俯冲于增生岛弧和东部陆块之下,镁铁质成岩物质来源于大洋板片重熔流体交代的岩石圈地幔楔,同时,对于华北地块新太古宙末期大陆地壳生长的时间提供约束。
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出版历程
收稿日期:  2015-12-29
修回日期:  2016-01-27
刊出日期:  2016-06-15

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