滇西腾冲曲石地区中更新世火山岩年龄及成因:SHRIMP锆石U-Pb定年和Hf同位素约束

李琳琳, 王书兵, 刘建辉, 石玉若. 滇西腾冲曲石地区中更新世火山岩年龄及成因:SHRIMP锆石U-Pb定年和Hf同位素约束[J]. 岩石学报, 2015, 31(9): 2609-2619.
引用本文: 李琳琳, 王书兵, 刘建辉, 石玉若. 滇西腾冲曲石地区中更新世火山岩年龄及成因:SHRIMP锆石U-Pb定年和Hf同位素约束[J]. 岩石学报, 2015, 31(9): 2609-2619.
LI LinLin, WANG ShuBing, LIU JianHui, SHI YuRuo. Age and origin of Mid-Pleistocene volcanic rocks from Qushi in Tengchong area, western Yunnan Province: SHRIMP zircon U-Pb dating and constraint from Hf-in-zircon isotopes[J]. Acta Petrologica Sinica, 2015, 31(9): 2609-2619.
Citation: LI LinLin, WANG ShuBing, LIU JianHui, SHI YuRuo. Age and origin of Mid-Pleistocene volcanic rocks from Qushi in Tengchong area, western Yunnan Province: SHRIMP zircon U-Pb dating and constraint from Hf-in-zircon isotopes[J]. Acta Petrologica Sinica, 2015, 31(9): 2609-2619.

滇西腾冲曲石地区中更新世火山岩年龄及成因:SHRIMP锆石U-Pb定年和Hf同位素约束

  • 基金项目:

    本文受中国地质调查项目(1212011120165)、国家自然科学基金项目(41173065)和国土资源部公益性行业基金(201311116)联合资助.

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Age and origin of Mid-Pleistocene volcanic rocks from Qushi in Tengchong area, western Yunnan Province: SHRIMP zircon U-Pb dating and constraint from Hf-in-zircon isotopes

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  • 本文报道了腾冲曲石地区英安岩测年结果和该区火山岩样品的地球化学特征。英安岩(TC7)的SHRIMP锆石U-Pb年龄为0.41±0.01Ma(MSWD=1.18),属于中更新世,是迄今在国内测得的最年轻的高精度锆石U-Pb年龄。该区的火山岩具有高钾钙碱性的特点,为一套粗面玄武岩-玄武粗安岩-粗安岩-粗面岩以及玄武岩-安山岩-英安岩岩石组合。岩石富集LILE、LREE,相对亏损Nb、Ta、Ti等高场强元素,具有高的原始地幔标准化(Th/Nb)N比值(大于6)、低的Nb/La(小于1)和Nb/U比值(3~13),相对富集Zr,Zr/Y比值较高。这些地球化学特征明显区别于典型岛弧钙碱性火山岩。锆石Hf同位素分析结果显示εHf(t)值为-11.0~-1.5,变化较大;tDM1、tDM2分别为747~1115Ma、951~1437Ma,模式年龄远大于SHRIMP测定的锆石U-Pb年龄。腾冲火山岩喷发时该区属于大陆板内环境,该区火山岩与地壳混染的大陆玄武岩地球化学特征相类似,是幔源物质遭受壳源富集组分强烈混染的产物。
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收稿日期:  2014-04-03
修回日期:  2014-12-10
刊出日期:  2015-09-30

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