中国东部全新世火山的镭-钍同位素年代学

邹海波, 郭紫佩, 樊祺诚, 赵勇伟. 2020. 中国东部全新世火山的镭-钍同位素年代学. 岩石学报, 36(7): 1945-1952. doi: 10.18654/1000-0569/2020.07.01
引用本文: 邹海波, 郭紫佩, 樊祺诚, 赵勇伟. 2020. 中国东部全新世火山的镭-钍同位素年代学. 岩石学报, 36(7): 1945-1952. doi: 10.18654/1000-0569/2020.07.01
ZOU HaiBo, GUO ZiPei, FAN QiCheng, ZHAO YongWei. 2020. Holocene volcanoes from eastern China: Constraints from Ra/Th isotope disequilibrium. Acta Petrologica Sinica, 36(7): 1945-1952. doi: 10.18654/1000-0569/2020.07.01
Citation: ZOU HaiBo, GUO ZiPei, FAN QiCheng, ZHAO YongWei. 2020. Holocene volcanoes from eastern China: Constraints from Ra/Th isotope disequilibrium. Acta Petrologica Sinica, 36(7): 1945-1952. doi: 10.18654/1000-0569/2020.07.01

中国东部全新世火山的镭-钍同位素年代学

  • 基金项目:

    本文受国家自然科学基金项目(41973029)资助

详细信息
    作者简介:

    邹海波, 男, 1966年生, 教授, 研究领域包括地球化学、岩石学、火山学, E-mail:haibo.zou@gmail.com

  • 中图分类号: P317;P597.3

Holocene volcanoes from eastern China: Constraints from Ra/Th isotope disequilibrium

  • 活火山是指1万年来有过喷发历史的全新世火山。火山的高分辨年代学对火山灾害评估和火山分类具有重要意义。对于缺乏历史记载的全新世火山,直接对火山岩进行同位素定年很困难。本文利用具有高时间分辨率的镭-钍-铀非平衡确定中国东部年轻火山的年龄。根据镭-钍-铀同位素,海南岛的马鞍岭和雷虎岭是全新世火山(马鞍岭:4.3ka;雷虎岭:4.7ka);镜泊湖火山(4.9ka)也是全新世火山;龙岗火山存在晚更新世和全新世活动(7.0ka,15.0ka);大兴安岭阿尔山和诺敏河Ra/Th非平衡消失但230Th/238U非平衡显著,属于晚更新世喷发(阿尔山:63ka;诺敏河:71ka)。海南岛的马鞍岭火山、雷虎岭火山和东北地区的龙岗火山、镜泊湖火山,是4座活火山。至于东北地区的阿尔山和诺敏河火山是否是活火山,有待测试更多样品的Ra/Th同位素。五大连池老黑山和火烧山有历史喷发记录,这与它们都存在显著Ra/Th非平衡一致。五大连池老黑山和火烧山的岩浆滞留年龄分别小于4.2ka和3.2ka,岩浆上升速率>18~23m/y。

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  • 图 1 

    中国东北年轻火山群分布示意图(a, 据白志达等, 2012)和中国东南海南岛年轻火山分布图(b, 据Zou and Fan, 2010)

    Figure 1. 

    Distribution of young volcanic groups in NE China (a, after Bai et al., 2012) and distribution of young volcanic fields in Hainan Island in SE China (b, after Zou and Fan, 2010)

    图 2 

    全岩样品的硅-全碱投影图

    Figure 2. 

    Silica-total alkali plot

    图 3 

    利用Ra/Th非平衡和Th/U非平衡制约火山岩年龄的流程图

    Figure 3. 

    A flowchart to determine the ages of young volcanic rocks using Ra/Th disequilibrium and Th/U disequilibrium

    图 4 

    利用(226Ra/230Th) (a)和利用(230Th/238U) (b)计算火山岩年龄(据Zou et al., 2002)

    Figure 4. 

    Calculation of ages of igneous rocks from (226Ra/230Th) (a) and from (230Th/238U) (b) (after Zou et al., 2002)

    图 5 

    五大连池老黑山火烧山的Ra/Th非平衡

    Figure 5. 

    Ra/Th disequilibrium for Laoheishan and Huoshaoshan

    图 6 

    东北地区镜泊湖、龙岗、阿尔山和诺敏河火山的Ra/Th非平衡

    Figure 6. 

    Ra/Th disequilibrium for Jingpohu, Longgang, Aershan and Nuominhe volcanoes

    图 7 

    利用Ra/Th非平衡估算镜泊湖、龙岗、马鞍岭、雷虎岭的年龄

    Figure 7. 

    Use of Ra/Th disequilibrium to estimate ages for volcanic rocks from eastern China

    图 8 

    利用Th/U非平衡估算龙岗、阿尔山、诺敏河的年龄

    Figure 8. 

    Use of Th/U disequilibrium to estimate ages for volcanic rocks from eastern China

    图 9 

    海南岛的马鞍岭火山和雷虎岭火山的Ra/Th同位素

    Figure 9. 

    Ra/Th disequilibrium for Maanling and Leihuling volcanos from Hainan Island

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收稿日期:  2020-04-07
修回日期:  2020-05-30
刊出日期:  2020-07-01

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