Collaborative Research: Synthesizing arc-scale geochemical, petrologic, and geophysical datasets to investigate causes of volcanic diversity in the Cascade Arc

合作研究:综合弧级地球化学、岩石学和地球物理数据集,研究喀斯喀特弧火山多样性的原因

基本信息

  • 批准号:
    1948834
  • 负责人:
  • 金额:
    $ 10.39万
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Continuing Grant
  • 财政年份:
    2020
  • 资助国家:
    美国
  • 起止时间:
    2020-07-01 至 2024-06-30
  • 项目状态:
    已结题

项目摘要

Subduction zones – locations where one of the Earth’s tectonic plates are pushed beneath another – are one of the most volcanically active environments on the planet. Decades of study on subduction zones have provided insight into the overarching processes that produce the magmas erupted, how the erupted magmas are produced at individual volcanoes, and a number of related questions. Despite this progress, a complex and largely unsolved problem is the cause of ubiquitous and dramatic variations in the amount and composition of magmas that erupt at volcanoes within the same subduction zone. Do these reflect processes acting deep within the Earth’s mantle, or in the overlying crust? Addressing this problem has important implications for understanding magma production and volcanic hazards, as worldwide almost a billion people live at risk from volcanoes. There is also a potential for scientific breakthrough by utilizing the existing large data sets acquired from recent NSF investments such as the MARGINS, GeoPRISMS, and EarthScope programs. However, addressing the question has proven challenging to date in part because of a lack of critical data for some locations, but largely because of the lack of suitable tools and approaches that allow us to quantitatively synthesize and compare the existing large data sets. Thus, this is a multidisciplinary study to conduct a quantitative comparison of existing large geophysical and compositional datasets at the spatial scales of the entire Cascades subduction zone, linked through sets of common intensive variables such as heat and density, to determine the primary drivers of intra-arc magmatic diversity. Building on a successful Proof of Concept project that demonstrates the promise of the approach (Till et al., 2019), the project will test hypotheses about the relative roles of mantle magmatic flux vs. crustal characteristics and crustal magma storage depths in producing variations in erupted compositions and fluxes, and in controlling the geophysical state of the crust along strike in the Quaternary Cascades arc. The project has the potential to transform our understanding of these important regions and will produce a number of important broader impacts including, catalyzing interdisciplinary collaborations between three PI’s at three institutions, producing expert datasets widely and easily available to the Earth Science community, supporting undergraduate experiential learning activities. Specifically, it will implement a new multi-year undergraduate research program CONVEcT program (Central Oregon Network for Volcano Education and Training) with research cohorts from Arizona State, Oregon State and Cornell Universities.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
俯冲带是地球上一个构造板块被推到另一个板块之下的地方,是地球上火山活动最活跃的环境之一。几十年来对俯冲带的研究已经深入了解了产生岩浆喷发的总体过程,喷发的岩浆是如何在各个火山产生的,以及一些相关的问题。尽管取得了这一进展,但一个复杂且基本上未解决的问题是,同一俯冲带内火山喷发的岩浆的数量和成分普遍存在巨大差异的原因。这些反映的是地幔深处的作用过程,还是上覆地壳的作用过程?解决这个问题对于了解岩浆的产生和火山的危害具有重要意义,因为全世界近10亿人生活在火山的危险之中。通过利用NSF最近投资获得的现有大型数据集,如MARGINS,GeoPRISMS和EarthScope计划,也有可能实现科学突破。然而,迄今为止,解决这一问题已被证明具有挑战性,部分原因是缺乏一些地点的关键数据,但主要是因为缺乏适当的工具和方法,使我们能够定量综合和比较现有的大型数据集。因此,这是一个多学科的研究,进行定量比较现有的大型地球物理和成分数据集在整个级联俯冲带的空间尺度,通过一套共同的密集变量,如热量和密度,以确定弧内岩浆多样性的主要驱动因素。基于一个成功的概念验证项目,该项目展示了该方法的前景(Till等人,2019年),该项目将测试有关地幔岩浆通量与地壳特征和地壳岩浆储存深度的相对作用的假设,以产生喷发成分和通量的变化,并控制第四纪级联弧中地壳沿着走向的地球物理状态。该项目有可能改变我们对这些重要区域的理解,并将产生许多重要的更广泛的影响,包括催化三个机构的三个PI之间的跨学科合作,生成地球科学界广泛且易于使用的专家数据集,支持本科生体验式学习活动。具体而言,它将实施一个新的多年本科研究计划CONVEcT计划(中央俄勒冈州火山教育和培训网络),来自亚利桑那州,俄勒冈州和康奈尔大学的研究队列。该奖项反映了NSF的法定使命,并被认为值得通过使用基金会的智力价值和更广泛的影响审查标准进行评估来支持。

项目成果

期刊论文数量(1)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Segmentation and Radial Anisotropy of the Deep Crustal Magmatic System Beneath the Cascades Arc
  • DOI:
    10.1029/2022gc010738
  • 发表时间:
    2023-03
  • 期刊:
  • 影响因子:
    3.7
  • 作者:
    Chengxin Jiang;B. Schmandt;G. Abers;E. Kiser;M. Miller
  • 通讯作者:
    Chengxin Jiang;B. Schmandt;G. Abers;E. Kiser;M. Miller
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Geoffrey Abers其他文献

Geoffrey Abers的其他文献

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{{ truncateString('Geoffrey Abers', 18)}}的其他基金

Systematic mapping of magma bodies under Cascades volcanoes
喀斯喀特火山下岩浆体的系统制图
  • 批准号:
    2313452
  • 财政年份:
    2023
  • 资助金额:
    $ 10.39万
  • 项目类别:
    Standard Grant
Collaborative Research: Investigating intraplate melting processes in northwest New Zealand with seismic imaging
合作研究:利用地震成像研究新西兰西北部的板内熔融过程
  • 批准号:
    2241063
  • 财政年份:
    2023
  • 资助金额:
    $ 10.39万
  • 项目类别:
    Continuing Grant
Collaborative Research: RAPID: Response to the 29 July 2021 Chignik M8.2 Earthquake
合作研究:RAPID:对 2021 年 7 月 29 日奇格尼克 M8.2 地震的响应
  • 批准号:
    2147438
  • 财政年份:
    2021
  • 资助金额:
    $ 10.39万
  • 项目类别:
    Standard Grant
Collaborative Research: Behavior and structure on and around the megathrust revealed by the Alaska Amphibious Seismic Community Experiment
合作研究:阿拉斯加两栖地震社区实验揭示的巨型逆冲断层及其周围的行为和结构
  • 批准号:
    1949130
  • 财政年份:
    2020
  • 资助金额:
    $ 10.39万
  • 项目类别:
    Standard Grant
Collaborative research: Structure and dynamics of the Alaska mantle wedge
合作研究:阿拉斯加地幔楔的结构和动力学
  • 批准号:
    1829440
  • 财政年份:
    2018
  • 资助金额:
    $ 10.39万
  • 项目类别:
    Standard Grant
Alaska Amphibious Community Seismic Experiment
阿拉斯加两栖社区地震实验
  • 批准号:
    1654568
  • 财政年份:
    2017
  • 资助金额:
    $ 10.39万
  • 项目类别:
    Standard Grant
Collaborative Research: Fate and Consequences of Yakutat Terrane Subduction Beneath Eastern Alaska and the Wrangell Volcanic Field
合作研究:阿拉斯加东部和兰格尔火山场下雅库塔特地体俯冲的命运和后果
  • 批准号:
    1460291
  • 财政年份:
    2015
  • 资助金额:
    $ 10.39万
  • 项目类别:
    Continuing Grant
Thermal and melt structure of the Juan de Fuca plate from ridge to trench to arc, inferred from seismic attenuation across the Amphibious Array
根据两栖阵列的地震衰减推断,胡安德富卡板块从山脊到海沟再到弧线的热结构和熔体结构
  • 批准号:
    1536566
  • 财政年份:
    2015
  • 资助金额:
    $ 10.39万
  • 项目类别:
    Standard Grant
MARGINS: Collaborative Research: Illuminating the Architecture of the Greater Mount St. Helens Magmatic System from Slab to Surface
边缘:合作研究:阐明大圣海伦斯山岩浆系统从板块到地表的结构
  • 批准号:
    1444275
  • 财政年份:
    2014
  • 资助金额:
    $ 10.39万
  • 项目类别:
    Continuing Grant
Collaborative Research: the role of fluids in intermediate-depth seismicity and wedge anisotropy: Case studies for Cascadia and Alaska, with a comparison to Japan
合作研究:流体在中深度地震活动和楔形各向异性中的作用:卡斯卡迪亚和阿拉斯加的案例研究,并与日本进行比较
  • 批准号:
    1446970
  • 财政年份:
    2014
  • 资助金额:
    $ 10.39万
  • 项目类别:
    Standard Grant

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