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西藏班公湖—怒江缝合带中段东巧地幔橄榄岩岩石成因及构造环境分析

董玉飞, 杨经绥, 连东洋, 熊发挥, 赵慧, 陈晓坚, 李观龙, 王天泽. 2019. 西藏班公湖—怒江缝合带中段东巧地幔橄榄岩岩石成因及构造环境分析[J]. 中国地质, 46(1): 87-114. doi: 10.12029/gc20190106
引用本文: 董玉飞, 杨经绥, 连东洋, 熊发挥, 赵慧, 陈晓坚, 李观龙, 王天泽. 2019. 西藏班公湖—怒江缝合带中段东巧地幔橄榄岩岩石成因及构造环境分析[J]. 中国地质, 46(1): 87-114. doi: 10.12029/gc20190106
DONG Yufei, YANG Jingsui, LIAN Dongyang, XIONG Fahui, ZHAO Hui, CHEN Xiaojian, LI Guanlong, WANG Tianze. 2019. Genesis and tectonic setting of the Dongqiao peridotites in the central segment of the Bangong Co-Nujiang Suture Zone[J]. Geology in China, 46(1): 87-114. doi: 10.12029/gc20190106
Citation: DONG Yufei, YANG Jingsui, LIAN Dongyang, XIONG Fahui, ZHAO Hui, CHEN Xiaojian, LI Guanlong, WANG Tianze. 2019. Genesis and tectonic setting of the Dongqiao peridotites in the central segment of the Bangong Co-Nujiang Suture Zone[J]. Geology in China, 46(1): 87-114. doi: 10.12029/gc20190106

西藏班公湖—怒江缝合带中段东巧地幔橄榄岩岩石成因及构造环境分析

  • 基金项目:
    国家自然科学基金项目(41720104009)、中国地质调查局项目(DD20160023-01)和部行业基金项目(201511022)联合资助
详细信息
    作者简介: 董玉飞, 男, 1994年生, 硕士生, 矿物学、岩石学、矿床学专业; E-mail:dongyufeisyq@163.com
    通讯作者: 杨经绥, 男, 1950年生, 中国科学院院士, 从事青藏高原和造山带的岩石大地构造研究; E-mail:yangjsui@163.com
  • 中图分类号: P588.12+5

Genesis and tectonic setting of the Dongqiao peridotites in the central segment of the Bangong Co-Nujiang Suture Zone

  • Fund Project: Supported by National Natural Science Foundation of China (No. 41720104009), China Geology Survey Project (No. DD20160023-01) and Foundation of MLR (No. 201511022)
More Information
    Author Bio: DONG Yufei, male, born in 1994, master candidate, majors in mineralogy, petrology and metallogeny; E-mail:dongyufeisyq@163.com .
    Corresponding author: YANG Jingsui, male, born in 1950, academician of the Chinese Academy of Sciences, majors in petrotectonics of Tibet and orogenic belt; E-mail:yangjsui@163.com
  • 东巧蛇绿岩位于班公湖—怒江缝合带中段,根据地理位置特征并以强玛镇为中心将东巧岩体划分为东西两个岩体。其中西岩体相对面积较大,由地幔橄榄岩、枕状玄武岩、辉长辉绿岩等组成;而东岩体面积较小,仅含地幔橄榄岩部分,各个不同单元之间呈断层接触关系。对东巧地幔橄榄岩开展岩石学、矿物学及地球化学研究发现:(1)东巧地幔橄榄岩以方辉橄榄岩为主,纯橄岩所占比例较小,约15%。豆荚状铬铁矿主要呈条带浸染状赋存在厚层且延伸较远的纯橄岩中。(2)东巧地幔橄榄岩中单斜辉石含量小于3%,矿物地球化学和全岩地球化学特征显示其来源于尖晶石相地幔源区的部分熔融,且部分熔融程度较高,估算在22%~28%,高于深海地幔橄榄岩的部分熔融程度(10%~22%)。(3)东巧地幔橄榄岩中的副矿物铬尖晶石Cr#值较高大于60,全岩具有U型球粒陨石标准化稀土元素配分模式,同时Rb、U、Zr和Sr相对富集,Hf和Nb相对亏损。全岩的地球化学特征指示了俯冲带之上的残余地幔与流体/熔体发生了反应,致使轻稀土元素以及部分微量元素选择性富集。综合东巧地幔橄榄岩的矿物化学组成成分以及全岩的地球化学特征,认为东巧地幔橄榄岩形成于大洋中脊的扩张环境中,后受到洋内俯冲作用的影响,导致俯冲带之上高度部分熔融的地幔橄榄岩与流体/熔体发生相互作用。

  • 加载中
  • 图 1  西藏班公湖—怒江缝合带蛇绿岩分布简图(据Liu et al., 2016)

    Figure 1. 

    图 2  班公湖—怒江缝合带中段东巧蛇绿岩地质简图(据西藏自治区地质矿产勘查开发局第五地质大队,2016简化)

    Figure 2. 

    图 3  东巧蛇绿岩中不同的地幔橄榄岩类型以及铬铁矿矿体产出特征

    Figure 3. 

    图 4  东巧地幔橄榄岩显微照片及背散射图像(图j~l)

    Figure 4. 

    图 5  东巧地幔橄榄岩橄榄石成分图解

    Figure 5. 

    图 6  东巧地幔橄榄岩斜方辉石成分图解(据Lian et al., 2016)

    Figure 6. 

    图 7  东巧地幔橄榄岩单斜辉石成分图解(据Lian et al., 2016)

    Figure 7. 

    图 8  东巧地幔橄榄岩尖晶石成分图解(据Pearce et al., 2000; Tamura and Aria, 2006; Lian et al., 2016)

    Figure 8. 

    图 9  东巧地幔橄榄岩全岩Al2O3/SiO2-MgO/SiO2图解(据Lian et al., 2016)

    Figure 9. 

    图 10  东巧、班公湖、罗布莎地幔橄榄岩球粒陨石标准化稀土元素配分图(标准化值据McDonough and Sun, 1995; 据Lian et al., 2016)

    Figure 10. 

    图 11  东巧、班公湖、罗布莎地幔橄榄岩原始地幔标准化微量元素蜘蛛图(标准化值据McDonough and Sun, 1995; 罗布莎数据据徐向珍, 2009;班公湖数据据史仁灯, 2005)

    Figure 11. 

    图 12  东巧地幔橄榄岩Tb/Yb-Al2O3图解(据Krishnakanta Singh, 2013)

    Figure 12. 

    图 13  东巧蛇绿岩中地幔橄榄岩Sc-Ni(a);Al2O3-Ni(b);Ti-Ni(c);Zr-Ni(d)图解(据Pearce et al., 2000)

    Figure 13. 

    表 1  东巧地幔橄榄岩中橄榄石的电子探针分析结果(部分数据)(%)

    Table 1.  Representative microprobe analyses of olivines from the Dongqiao mantle peridotites(%)

    下载: 导出CSV

    表 2  东巧地幔橄榄岩中斜方辉石的电子探针分析结果(部分数据)(%)

    Table 2.  Representative microprobe analyses of orthopyroxenes from the Dongqiao mantle peridotites(%)

    下载: 导出CSV

    表 3  东巧地幔橄榄岩中单斜辉石的电子探针分析结果(部分数据)(%)

    Table 3.  Representative microprobe analyses of clinopyroxenes from the Dongqiao mantle peridotites(%)

    下载: 导出CSV

    表 4  东巧地幔橄榄岩中铬尖晶石的电子探针分析结果(部分数据)(%)

    Table 4.  Representative microprobe analyses of spinels from the Dongqiao mantle peridotites(%)

    下载: 导出CSV

    表 5  东巧蛇绿岩地幔橄榄岩全岩地球化学分析数据(主量元素/%,稀土元素和微量元素/10−6)

    Table 5.  Whole rock composition of Dongqaio peridotites (Major elements: wt%; Rare Earth Elements and trace elements: ×10−6)

    下载: 导出CSV
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出版历程
收稿日期:  2018-08-02
修回日期:  2019-01-23
刊出日期:  2019-02-25

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