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Collaborative Research: Plutons as ingredients for continental crust: Pilot study of the differences between intermediate plutons and lavas in the intra-oceanic Aleutian arc

Collaborative Research: Plutons as ingredients for continental crust: Pilot study of the differences between intermediate plutons and lavas in the intra-oceanic Aleutian arc
合作研究:岩体作为大陆地壳的成分:对大洋内阿留申弧中的中间岩体和熔岩之间差异的初步研究
批准号:
1144759
负责人:
Peter Kelemen
金额:
$9.91万
依托单位:
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2012
资助国家:
美国
项目状态:
已结题
起止时间:
2012-02-15 至 2014-07-31

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中文摘要
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英文摘要
Felsic plutonic rocks formed in arcs are buoyant with respect to mantle peridotite over the entire range of relevant pressures and temperatures. They tend to remain at the Earth?s surface, to form the fundamental building blocks of continental crust. In the Aleutians, most felsic plutonic rocks have compositions that overlap estimates for the bulk composition of the continental crust, and that are distinctly different from spatially associated lavas. Understanding the genesis of Aleutian felsic plutonic rocks is a key to understanding continental genesis and evolution via arc magmatism, a key science goal for the MARGINS and GeoPRISMS Initiatives. The PIs will address the following questions: (1) Do Aleutian plutonic rocks have an isotopically distinct source composition, compared to nearby lavas? If they do, this is vitally important since it is commonly assumed that erupted basalts are representative of the magmatic flux from the mantle into arc crust. If not, we will evaluate how they can be explained as the result of different differentiation processes operating on the same parental melt. (2) Has there been compositional variation in the Aleutian arc over time? Do differences between plutonic and volcanic rocks represent temporal evolution of the arc, or different modes of magma transport and emplacement for different magma compositions? And (3) are high viscosity felsic magmas preferentially emplaced in plutons, while low viscosity, mafic magmas preferentially form lavas? What biases does this introduce, when lavas are presumed to be representative of arc magmatic processes and compositions?Broader Impacts: The Aleutian arc poses numerous hazards to society. Understanding subduction processes helps to predict, avoid, and/or mitigate the hazardous consequences of volcanic eruptions, landslides and earthquakes. During this project, a graduate student will be trained in research, and will likely be able to help design and participate in a larger field research program based on this pilot project.
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Collaborative Research: Focused Study of Aleutian Plutons and their Host Rocks: Understanding the building blocks of continental crust
  • 批准号:
    1457293
  • 项目类别:
    Standard Grant
  • 资助金额:
    $20.0万
  • 财政年份:
    2015
  • 负责人:
    Peter Kelemen
  • 依托单位:
Collaborative Research: Alteration of mantle peridotite: Geochemical fluxes and dynamics of far from equilibrium transport
  • 批准号:
    1516300
  • 项目类别:
    Standard Grant
  • 资助金额:
    $196.84万
  • 财政年份:
    2015
  • 负责人:
    Peter Kelemen
  • 依托单位:
2012 Rock Deformation Gordon Research Conference: Feedback Processes in Rock Deformation
  • 批准号:
    1238362
  • 项目类别:
    Standard Grant
  • 资助金额:
    $2.25万
  • 财政年份:
    2012
  • 负责人:
    Peter Kelemen
  • 依托单位:
Petrologic Study of Peridotite Carbonation in Oman: Temperature, Timing and Fluid Composition
  • 批准号:
    1049905
  • 项目类别:
    Standard Grant
  • 资助金额:
    $30.02万
  • 财政年份:
    2011
  • 负责人:
    Peter Kelemen
  • 依托单位:
国内基金
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Research on Quantum Field Theory without a Lagrangian Description
  • 批准号:
    24ZR1403900
  • 项目类别:
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  • 资助金额:
    --
  • 批准年份:
    2024
  • 负责人:
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  • 依托单位:
Cell Research
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