Identifying Crustal and Mantle Processes in the Central Trans-Mexican Volcanic Belt

识别跨墨西哥火山带中部的地壳和地幔过程

基本信息

  • 批准号:
    1019798
  • 负责人:
  • 金额:
    $ 27.75万
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Continuing Grant
  • 财政年份:
    2010
  • 资助国家:
    美国
  • 起止时间:
    2010-09-15 至 2015-08-31
  • 项目状态:
    已结题

项目摘要

Intellectual Merit: Subduction zones are the sites of much of the Earth's active explosivevolcanism and associated hazards, and also important sites of mass exchange between the crust and mantle, and fundamental agents in the growth of the continental crust and evolution of the crust-mantle system through time. Much attention has been focused on explosive silicicstratovolcanoes, yet less studied mafic monogenetic cones are very common and can be highly destructive. In addition, their mafic composition makes them ideal for study of mantle processes in subduction settings. We propose to do a detailed multi-isotopic study of the historic Jorullo and Parícutin monogenetic volcanic centers in the central Trans-Mexican Volcanic Belt. Jorullo and Parícutin volcanoes are ideal for a paired case study because: they both produced well documented historic eruptions; detailed field studies have been done so samples selected for geochemical analysis can be placed in stratigraphic context; they both exhibit a temporal compositional trend of increasing SiO2 with time that is common in mafic monogenetic eruptions but the origin of which is poorly understood; they represent possible endmembers in inferred extents of crustal interaction, with lesser contamination of Jorullo lavas and very extensive contamination of Parícutin lavas; existing local upper and lower crustal xenoliths will allow rigorous investigation of the role of lithospheric assimilation; and their close geographic proximity enables a comparison of potential variability of mantle and crustal processes in different volcanic centers in a relatively fixed tectonic/geologic setting. Sr-Nd-Pb-Hf-Os isotopic compositions will be measured on whole-rock lavas, tephra, and crustal xenoliths, O and Os isotopes on olivine-oxide-matrix separates, and Sr isotopes in single melt-inclusion-bearing olivines. These data should uniquely constrain the relative roles of lower and upper crustal assimilation and the potential addition of slab-derived components to the mantle wedge including hydrous slab-fluid and sediment-melt. This study will have important implications regarding the establishment of magma reservoirs in mafic monogenetic volcanic systems and the cause of temporal-compositional variations in eruptive products, and will provide insights into the nature and heterogeneities of slab-derived fluids/melts over small spatial scales within a mantle wedge.Broader Impacts: Student Training & Education: Students involved in this project will gain extensive experience in several state-of-the-art analytical techniques, and at least one student will participate in fieldwork, receiving training in field volcanology. It is anticipated that the field work will be done in conjunction with a volcanology field workshop, providing the opportunity for additional students to benefit. Results from this research will also be incorporated into the classroom in lecture material and related hands-on, inquiry-based learning activities. Mentoring Women in Science: Widom serves as a role model/mentor for women in science, and currently has a research group with 4 female Ph.D. students. Widom and her students have worked closely with undergraduates in the past, and it is anticipated that the female-dominated research group will help attract participation of female undergraduate students. Outreach Activities: This project will be closely linked to the recent von Humboldt Foundation grant to Siebe and Schmincke, in which results of field mapping and volcanological studies, and our new geochemical data, will be integrated with the establishment of Jorullo as a new UNESCO GeoPark. In addition, Widom and her students will be involved in outreach programs through Miami U, including serving as consultants with Miami's Limper Geology Museum and providing research-based educational experiences to the community through the museum's K-12 programs as well as lab tours/demonstrations to local retirees and community college students. Volcanic Hazard Assessment: The results of this project will help constrain pre-eruptive processes in two historic volcanoes in a highly active volcanic region in which any future eruption will have a major impact on the local population and major urban centers including Morelia and likely Mexico City. International Collaboration: This project will foster ongoing international collaborations with Mexican geologists Siebe and Schaaf, as well as German volcanologist Schmincke.This award is co-funded by the Office of International Science and Engineering (OISE).
智力优势:俯冲带是地球上许多活跃的爆发性火山活动和相关灾害的发生地,也是地壳和地幔之间物质交换的重要场所,也是大陆地壳生长和壳幔系统随时间演化的基本因素。很多注意力都集中在爆炸性硅质层火山上,但研究较少的镁铁质单生火山锥非常常见,并且具有高度破坏性。此外,它们的镁铁质成分使它们成为研究俯冲环境中地幔过程的理想选择。我们建议对跨墨西哥火山带中部历史悠久的 Jorullo 和 Parícutin 单生火山中心进行详细的多同位素研究。乔鲁洛火山和帕里库廷火山是配对案例研究的理想选择,因为: 它们都产生了有据可查的历史喷发;已经进行了详细的实地研究,以便可以将选定用于地球化学分析的样本置于地层背景中;它们都表现出 SiO2 随着时间的推移而增加的时间成分趋势,这在镁铁质单成岩喷发中很常见,但对其起源知之甚少;它们代表了推断的地壳相互作用范围内可能的端元,其中 Jorullo 熔岩的污染程度较小,Parícutin 熔岩的污染范围非常广泛;现有的当地上地壳和下地壳捕虏体将允许对岩石圈同化的作用进行严格的研究;它们的地理接近性使得能够在相对固定的构造/地质环境中比较不同火山中心的地幔和地壳过程的潜在变化。将测量全岩熔岩、火山灰和地壳捕虏体上的 Sr-Nd-Pb-Hf-Os 同位素组成,测量橄榄石氧化物基质分离物上的 O 和 Os 同位素,以及含有单一熔体包裹体的橄榄石中的 Sr 同位素。这些数据应该独特地限制了下地壳和上地壳同化的相对作用,以及板片衍生成分向地幔楔的潜在添加,包括含水板片流体和沉积物熔体。这项研究将对镁铁质单成因火山系统中岩浆储层的建立以及喷发产物的时间成分变化的原因产生重要影响,并将深入了解地幔楔内小空间尺度上板片衍生的流体/熔体的性质和非均质性。 更广泛的影响:学生培训和教育:参与该项目的学生将在多个方面获得丰富的经验 最先进的分析技术,至少一名学生将参加实地工作,接受野外火山学培训。预计现场工作将与火山学现场研讨会结合进行,为更多学生提供受益的机会。这项研究的结果也将被纳入课堂的讲座材料和相关的实践、探究性学习活动中。指导科学界女性:Widom 是科学界女性的榜样/导师,目前拥有一个由 4 名女性博士组成的研究小组。学生。 Widom 和她的学生过去与本科生密切合作,预计以女性为主的研究小组将有助于吸引女本科生的参与。外展活动:该项目将与冯·洪堡基金会最近向 Siebe 和 Schmincke 提供的资助密切相关,其中实地测绘和火山学研究的结果以及我们新的地球化学数据将与乔鲁洛作为新的联合国教科文组织地质公园的建立相结合。此外,Widom 和她的学生将参与迈阿密大学的外展项目,包括担任迈阿密林珀地质博物馆的顾问,通过博物馆的 K-12 项目向社区提供基于研究的教育经验,以及为当地退休人员和社区学院的学生提供实验室参观/演示。火山危害评估:该项目的结果将有助于限制位于高度活跃火山地区的两座历史悠久的火山的喷发前过程,该地区未来的任何喷发都将对当地人口和主要城市中心(包括莫雷利亚和可能的墨西哥城)产生重大影响。国际合作:该项目将促进与墨西哥地质学家 Siebe 和 Schaaf 以及德国火山学家 Schmincke 的持续国际合作。该奖项由国际科学与工程办公室 (OISE) 共同资助。

项目成果

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Elisabeth Widom其他文献

Assessment of tree bark as a biomonitor of anthropogenic thorium and radium contamination
Ancient mantle in a modern plume
现代地幔柱中的古老地幔
  • DOI:
    10.1038/420281a
  • 发表时间:
    2002-11-21
  • 期刊:
  • 影响因子:
    48.500
  • 作者:
    Elisabeth Widom
  • 通讯作者:
    Elisabeth Widom
Analysis of a sugar maple tree core for monitoring environmental uranium contamination
Long-term changes in particulate matter abundance and sources in an industrial city: Insights from microscopy and elemental and Pb isotopic compositions of bio-monitors
一座工业城市中颗粒物丰度及其来源的长期变化:来自生物监测器的显微镜观察以及元素和铅同位素组成的见解
  • DOI:
    10.1016/j.envpol.2025.126590
  • 发表时间:
    2025-09-15
  • 期刊:
  • 影响因子:
    7.300
  • 作者:
    Maral Khodadadi;Elisabeth Widom;Masoomeh Kousehlar;Mark P.S. Krekeler
  • 通讯作者:
    Mark P.S. Krekeler
Erratum to: Analysis of a sugar maple tree core for monitoring environmental uranium contamination

Elisabeth Widom的其他文献

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{{ truncateString('Elisabeth Widom', 18)}}的其他基金

Collaborative Research: Volcanism on the Edge - Basaltic Volcanism from Source to Surface across the Colorado Plateau/Basin & Range Transition in SW Utah
合作研究:边缘火山活动 - 科罗拉多高原/盆地从源头到地表的玄武岩火山活动
  • 批准号:
    2152696
  • 财政年份:
    2022
  • 资助金额:
    $ 27.75万
  • 项目类别:
    Standard Grant
Collaborative Research: Origin and Evolution of Intraplate Magmatism at the Revillagigedo Archipelago, Mexico
合作研究:墨西哥雷维拉吉赫多群岛板内岩浆作用的起源和演化
  • 批准号:
    2026799
  • 财政年份:
    2020
  • 资助金额:
    $ 27.75万
  • 项目类别:
    Continuing Grant
MRI: Acquisition of a Multi-Collector ICP-MS with Laser Ablation for Geochemical and Geochronological Applications
MRI:获取具有激光烧蚀功能的多接收器 ICP-MS,用于地球化学和地质年代学应用
  • 批准号:
    1919658
  • 财政年份:
    2019
  • 资助金额:
    $ 27.75万
  • 项目类别:
    Standard Grant
Collaborative Research: Testing Source vs. Crustal Processing in High-Mg# Arc Magmas by Os-O-He-Olivine Systematics
合作研究:高镁测试来源与地壳处理
  • 批准号:
    1921643
  • 财政年份:
    2019
  • 资助金额:
    $ 27.75万
  • 项目类别:
    Standard Grant
From Cones to Clusters: Evolution of a Monogenetic Volcanic Field
从锥体到簇状:单生火山场的演化
  • 批准号:
    1853006
  • 财政年份:
    2019
  • 资助金额:
    $ 27.75万
  • 项目类别:
    Standard Grant
Origin & Eruptive History of Quaternary Volcanism in Nosy Be and Itasy-Ankaratra, Madagascar
起源
  • 批准号:
    1523442
  • 财政年份:
    2015
  • 资助金额:
    $ 27.75万
  • 项目类别:
    Standard Grant
Collaborative Research: Links Between Magma Source Characteristics, Shallow Plumbing, and Eruptive Styles in Mafic Intraplate Volcanic Fields (Lunar Crater Volcanic Field, Nevada)
合作研究:岩浆源特征、浅层管道和镁铁质板内火山田喷发类型之间的联系(内华达州月球陨石坑火山田)
  • 批准号:
    1016042
  • 财政年份:
    2010
  • 资助金额:
    $ 27.75万
  • 项目类别:
    Standard Grant
Constraining Processes & Timescales of Magma Evolution
约束流程
  • 批准号:
    0911182
  • 财政年份:
    2009
  • 资助金额:
    $ 27.75万
  • 项目类别:
    Standard Grant
Technician Support: Management of Thermal Ionization Mass Spectrometry and Isotope Geochemistry Clean Labs
技术人员支持:热电离质谱和同位素地球化学洁净实验室的管理
  • 批准号:
    0622267
  • 财政年份:
    2007
  • 资助金额:
    $ 27.75万
  • 项目类别:
    Continuing Grant
Acquisition of a Microwave Digestion System for Geochemical and Geochronological Applications
获取用于地球化学和地质年代学应用的微波消解系统
  • 批准号:
    0549552
  • 财政年份:
    2006
  • 资助金额:
    $ 27.75万
  • 项目类别:
    Standard Grant

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Improved Constraints on Mantle and Crustal Source Signals in CO2 well gases: New Insights from Ultra-high Precision Noble Gas and Clumped Isotope Measurements
改进对 CO2 井气体中地幔和地壳源信号的约束:超高精度稀有气体和聚集同位素测量的新见解
  • 批准号:
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EAGER: Collaborative Research: Mantle fluid contribution to springs along the Denali Fault System: Constraints on the crustal scale nature of the main strand and splays
EAGER:合作研究:地幔流体对德纳里断层系统沿线泉水的贡献:对主链和斜张地壳尺度性质的限制
  • 批准号:
    2016336
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Insight into early craton nucleation and stabilization – a case study from crustal and mantle xenoliths from the Star kimberlite mine, East Kaapvaal craton
深入了解早期克拉通成核和稳定——来自东卡普瓦尔克拉通 Star 金伯利岩矿的地壳和地幔捕虏体的案例研究
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    448405043
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    2020
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EAGER: Collaborative Research: Mantle fluid contribution to springs along the Denali Fault System: Constraints on the crustal scale nature of the main strand and splays
EAGER:合作研究:地幔流体对德纳里断层系统沿线泉水的贡献:对主链和斜张地壳尺度性质的限制
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Crustal and Uppermost Mantle Anisotropy Across Tibet and East China
西藏和中国东部的地壳和上地幔各向异性
  • 批准号:
    1645269
  • 财政年份:
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Isotopic studies of crustal and mantle evolution
地壳和地幔演化的同位素研究
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    121767-2013
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Next-generation 3D imaging of the on- and off-axis mantle and crustal magmatic systems at the Endeavour segment
Endeavour 段的轴上和离轴地幔和地壳岩浆系统的下一代 3D 成像
  • 批准号:
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