Collaborative Research: Investigating out-of sequence magmatism and mantle plume-lithosphere interactions adjacent to the Snake River plain (U.S.A.)

合作研究:调查蛇河平原附近的无序岩浆作用和地幔柱-岩石圈相互作用(美国)

基本信息

  • 批准号:
    2002786
  • 负责人:
  • 金额:
    $ 21.38万
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Standard Grant
  • 财政年份:
    2020
  • 资助国家:
    美国
  • 起止时间:
    2020-09-01 至 2023-08-31
  • 项目状态:
    已结题

项目摘要

Volcanic eruptions are significant hazards and drivers of societal and environmental change. Continental hotspot eruptions are the soures of the largest documented eruptions on Earth. Hotspot magmatism is recognized in part on identification of a linear chain of volcanoes that becomes younger opposite the direction of plate motion. These age-progressions may be unclear when volcanism along a hotspot “track” does not temporally fit in the age progression and is therefore, out of sequence and at times, off-axis. The Snake River Plain-Yellowstone (SRPY) volcanic province (Wyoming-Montana-Idaho, including Yellowstone National Park) is the classic example of continental hotspot magmatism, and major SRPY “supervolcano” eruptions are well documented. Small-volume volcanoes exist adjacent to the SRPY, however. This project will investigate these out of sequence volcanoes to provide an analog to better identify hotspots in the geological record, yield new constraints on how the Yellowstone hotspot interacts with North America, and be used to help refine models for the origin and eruptive history of volcanism associated with this hotspot. The findings have implications for continental hotspot volcanic hazard assessments. Student training and public outreach are also key aspects of this project. A multidisciplinary approach will be employed to unravel the spatial-temporal magmatic history adjacent to the youngest part of the SRPY hotspot track, including field mapping focused on the relations between structures and igneous activity, geochronology, and geochemistry. These data will allow the research team to: [1] determine the temporal-spatial history of out-of-sequence volcanism adjacent to the SRPY; [2] define the mantle and crustal contributions to this out of sequence and off-axis volcanism; [3] decipher the links between syn-magmatic extension, SRPY magmatism and the out of sequence and off-axis volcanism. The proposed study will provide opportunities for undergraduate and graduate students to learn a diverse suite of field, presentation, and laboratory skills. Curriculum for GeoFORCE, a Native Alaskan STEM education program, will be created and taught. GeoFORCE participants shall visit Yellowstone National Park. Scientific advances made during this project will be communicated to the public via collaboration with the Dubois Museum through public talks and field trips, the development of a geological guide of the upper Wind River basin (WY), and via news articles published globally on the web and in local newspapers.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.
火山喷发是社会和环境变化的重大危害和驱动因素。大陆热点喷发是地球上有记录的最大火山喷发的根源,部分是通过识别与板块运动方向相反的线性火山链来识别的。当沿着热点“轨迹”的火山活动在时间上不适合年龄进展时,这些年龄进展可能会不清楚,因此不按顺序,有时会偏离轴。斯内克河平原-黄石 (SRPY) 火山省(怀俄明州-蒙大拿州-爱达荷州,包括黄石国家公园)是大陆热点岩浆活动的典型例子,并且在其附近存在大型 SRPY“超级火山”喷发。然而,SRPY 项目将调查这些不按顺序排列的火山,以提供一个类比,以更好地识别地质记录中的热点,并产生新的限制。黄石热点与北美相互作用,可用于帮助完善与该热点相关的火山活动的起源和喷发历史模型。这些发现对大陆热点火山灾害评估具有重要意义。学生培训和公共宣传也是该项目的关键方面。将采用多学科方法来揭示与 SRPY 热点轨道最年轻部分相邻的时空岩浆历史,包括侧重于结构与火成岩活动之间关系的野外测绘,这些数据将使研究小组能够: [1] 确定 SRPY 附近无序火山活动的时空历史; [2] 定义地幔和地壳对这种无序火山活动的贡献;离轴火山活动;[3] 破译同岩浆延伸、SRPY 岩浆活动与无序和离轴火山活动之间的联系。拟议的研究将为本科生和学生提供机会。将为阿拉斯加原住民 STEM 教育计划 GeoFORCE 创建和教授各种现场、演示和实验室技能。 GeoFORCE 参与者将参观黄石国家公园,并交流该项目期间取得的科学进展。通过与杜波依斯博物馆合作,通过公开演讲和实地考察、开发风河流域上游 (WY) 地质指南,以及通过在全球网络和当地报纸上发表的新闻文章,向公众展示。该奖项反映了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,NSF 的法定使命被认为值得支持。

项目成果

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Jeff Benowitz其他文献

Geochronology and Tectonic Context of Lithium-Cesium-Tantalum Pegmatites In the Appalachians
阿巴拉契亚山脉锂铯钽伟晶岩的年代学和构造背景
  • DOI:
  • 发表时间:
    2016
  • 期刊:
  • 影响因子:
    0
  • 作者:
    D. Bradley;E. Shea;R. Buchwaldt;Sam Bowring;Jeff Benowitz;P. O’Sullivan;A. McCauley
  • 通讯作者:
    A. McCauley

Jeff Benowitz的其他文献

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{{ truncateString('Jeff Benowitz', 18)}}的其他基金

RII Track-4: Why are Young Volcanic Rocks Undateable: Chemistry, Environment, or Instrumentation?
RII Track-4:为什么年轻的火山岩无法测年:化学、环境或仪器?
  • 批准号:
    1833105
  • 财政年份:
    2018
  • 资助金额:
    $ 21.38万
  • 项目类别:
    Standard Grant
RII Track-4: Why are Young Volcanic Rocks Undateable: Chemistry, Environment, or Instrumentation?
RII Track-4:为什么年轻的火山岩无法测年:化学、环境或仪器?
  • 批准号:
    1833105
  • 财政年份:
    2018
  • 资助金额:
    $ 21.38万
  • 项目类别:
    Standard Grant
Collaborative Research: A four-dimensional view of deformation in the Eastern Alaska Range - where did the slip on the Denali fault go?
合作研究:阿拉斯加东部山脉变形的四维视图——德纳利断层上的滑动去了哪里?
  • 批准号:
    1828023
  • 财政年份:
    2018
  • 资助金额:
    $ 21.38万
  • 项目类别:
    Standard Grant
Collaborative Research: Investigating Controls on Temporal-spatial Heterogeneous Deformation Along a Transpressive Strike-slip Fault System: The Eastern Denali Fault Corner
合作研究:研究沿挤压走滑断层系统时空非均质变形的控制:东迪纳利断层角
  • 批准号:
    1550123
  • 财政年份:
    2016
  • 资助金额:
    $ 21.38万
  • 项目类别:
    Continuing Grant
Collaborative Research: Geological Constraints on ~25 Million Years of Magmatism Along an Arc-transform Junction, Wrangell Volcanic Belt, Alaska
合作研究:阿拉斯加兰格尔火山带弧形转换交界处约 2500 万年岩浆活动的地质约束
  • 批准号:
    1450730
  • 财政年份:
    2015
  • 资助金额:
    $ 21.38万
  • 项目类别:
    Standard Grant
Developing a tephra database to document the evolution of explosive volcanism along the Gulf of Alaska margin for the past six million years
开发火山灰数据库来记录过去六百万年阿拉斯加湾边缘爆发性火山活动的演变
  • 批准号:
    1434656
  • 财政年份:
    2014
  • 资助金额:
    $ 21.38万
  • 项目类别:
    Standard Grant
Collaborative Research: A Late Cenozoic Record of Restraining Bend Initiation and Evolution along the Denali Fault at Mount McKinley, Alaska
合作研究:阿拉斯加麦金利山德纳里断层沿新生代抑制弯曲起始和演化的记录
  • 批准号:
    1249885
  • 财政年份:
    2013
  • 资助金额:
    $ 21.38万
  • 项目类别:
    Standard Grant

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  • 批准号:
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