EAGER: Collaborative Research: Collaborative Investigations of Isotopic Fractionation by Thermal Diffusion and Thermal Migration

EAGER:协作研究:通过热扩散和热迁移进行同位素分馏的协作研究

基本信息

项目摘要

This EArly-concept Grant for Exploratory Research (EAGER) represents an interdisciplinary effort to address the geochemical processes that could be responsible for recent observations of stable isotope variations for "non-traditional stable isotopes" in igneous rocks (NTSI). Significant fractionations in the isotopes of Mg and Si are difficult to explain in terms of equilibrium between minerals and their melts during common igneous differentiation processes. The exciting new discovery that large isotopic fractionations occur in melts held within a temperature gradient offers a possible explanation for the observed isotope variations. The fractionation by thermal diffusion is so large that it may provide the basis for a unique tool to discern the role of thermal-gradient-driven processes for magmatic differentiation. This project represents a synergistic and novel collaboration that brings experimental, analytical, and theoretical approaches to the study of this NTSI fractionation phenomenon. Three complementary efforts will be undertaken that include: 1) Laboratory silicate Soret (fully molten) experiments using both natural compositions and selected simple systems; 2) Analysis of major and trace element behavior and NTSI fractionation in thermal migration (partially molten) experiments on basalt to rhyolite bulk compositions and determination of BetaT for Mg, Si and Fe; and 3) Molecular dynamics simulations of isotope fractionation within a temperature gradient in the MgO-SiO2 system to investigate the physical basis for the effects of thermal diffusion on NTSI fractionation. The proposed science plan brings together three groups of researchers with different expertises in petrology/geochemistry research from field petrology to experimental petrology to molecular dynamics simulation.
这个早期概念的探索性研究资助(EAGER)代表了一个跨学科的努力,以解决地球化学过程,可能是负责稳定同位素变化的火成岩(NTSI)中的“非传统稳定同位素”的最新观测。 Mg和Si同位素的显著分馏很难用矿物和熔体之间的平衡来解释。令人兴奋的新发现,大的同位素分馏发生在熔体内的温度梯度提供了一个可能的解释所观察到的同位素变化。热扩散分馏是如此之大,它可以提供一个独特的工具来辨别岩浆分异热梯度驱动过程的作用的基础。该项目代表了一种协同和新颖的合作,为NTSI分馏现象的研究带来了实验,分析和理论方法。 将开展三项补充工作,包括:1)实验室硅酸盐Soret利用天然组分和选定的简单体系进行的(全熔融)实验; 2)热迁移过程中主量和微量元素行为及NTSI分馏分析玄武岩到流纹岩整体成分的(部分熔融)实验和Mg、Si和Fe的BetaT测定;(3)MgO-SiO_2体系中温度梯度下同位素分馏的分子动力学模拟,探讨热扩散对NTSI分馏影响的物理基础。拟议的科学计划汇集了三组研究人员,他们在岩石学/地球化学研究方面具有不同的专业知识,从野外岩石学到实验岩石学再到分子动力学模拟。

项目成果

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Craig Lundstrom其他文献

Chemical and physical weathering in south Patagonian rivers: A combined Sr–U–Be isotope approach
  • DOI:
    10.1016/j.gca.2012.09.054
  • 发表时间:
    2013-01-15
  • 期刊:
  • 影响因子:
  • 作者:
    Borom Lee;Yeongcheol Han;Youngsook Huh;Craig Lundstrom;Lionel L. Siame;Jong Ik Lee;Byong-Kwon Park; ASTER Team
  • 通讯作者:
    ASTER Team
Plume–ridge interaction studied at the Galápagos spreading center: Evidence from <sup>226</sup>Ra–<sup>230</sup>Th–<sup>238</sup>U and <sup>231</sup>Pa–<sup>235</sup>U isotopic disequilibria
  • DOI:
    10.1016/j.epsl.2005.02.031
  • 发表时间:
    2005-05-30
  • 期刊:
  • 影响因子:
  • 作者:
    Thomas Find Kokfelt;Craig Lundstrom;Kaj Hoernle;Folkmar Hauff;Reinhard Werner
  • 通讯作者:
    Reinhard Werner
δ56Fe of magnetite as a tool for tracking mush-to-magma processes
δ56Fe 磁铁矿作为追踪糊状岩浆过程的工具
  • DOI:
  • 发表时间:
    2022
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Karoline M Bruckel;Craig Lundstrom
  • 通讯作者:
    Craig Lundstrom
<sup>231</sup>Pa systematics in postglacial volcanic rocks from Iceland
  • DOI:
    10.1016/j.gca.2015.12.011
  • 发表时间:
    2016-07-15
  • 期刊:
  • 影响因子:
  • 作者:
    Simon Turner;Thomas Kokfelt;Kaj Hoernle;Craig Lundstrom;Folkmar Hauff
  • 通讯作者:
    Folkmar Hauff

Craig Lundstrom的其他文献

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{{ truncateString('Craig Lundstrom', 18)}}的其他基金

Collaborative Research: Investigating formation of stagnant slabs and implications for subduction dynamics
合作研究:调查静止板片的形成及其对俯冲动力学的影响
  • 批准号:
    2244660
  • 财政年份:
    2023
  • 资助金额:
    $ 6万
  • 项目类别:
    Standard Grant
EAGER: Investigating the possibility of low temperature (<700 C) melt in silicic igneous systems
EAGER:调查低温的可能性(
  • 批准号:
    1919714
  • 财政年份:
    2019
  • 资助金额:
    $ 6万
  • 项目类别:
    Standard Grant
Integrating Experiments With Observations at Oldoinyo Lengai; Insights Into Alkalic Magmatic Processes
将 Oldoinyo Lengai 的实验与观察相结合;
  • 批准号:
    1427386
  • 财政年份:
    2014
  • 资助金额:
    $ 6万
  • 项目类别:
    Continuing Grant
Acquisition of a laser ablation system for the Department of Geology, UIUC
为 UIUC 地质系购置激光烧蚀系统
  • 批准号:
    1441465
  • 财政年份:
    2014
  • 资助金额:
    $ 6万
  • 项目类别:
    Standard Grant
Collaborative Research: Investigating MORB differentiation through non-traditional stable isotope analyses
合作研究:通过非传统稳定同位素分析研究 MORB 分化
  • 批准号:
    1060754
  • 财政年份:
    2011
  • 资助金额:
    $ 6万
  • 项目类别:
    Standard Grant
Collaborative Proposal: Integrated Investigations of Isotope Fractionation in Magmatic Systems
合作提案:岩浆系统中同位素分馏的综合研究
  • 批准号:
    1019632
  • 财政年份:
    2010
  • 资助金额:
    $ 6万
  • 项目类别:
    Standard Grant
Collaborative Research: Probing mantle plumbing beneath Pacific ridges thriugh study of the Lamont and Vance Seamount chains
合作研究:通过拉蒙特海山链和万斯海山链的研究来探测太平洋海脊下的地幔管道
  • 批准号:
    0825612
  • 财政年份:
    2008
  • 资助金额:
    $ 6万
  • 项目类别:
    Standard Grant
Assessing Diffusive Differentiation During Igneous Intrusion Using Integrated Theoretical, Experimental and Field Studies
利用综合理论、实验和现场研究评估火成岩侵入过程中的扩散分异
  • 批准号:
    0609726
  • 财政年份:
    2006
  • 资助金额:
    $ 6万
  • 项目类别:
    Continuing Grant
Collaborative Research: Investigating the Processes and Timescales of Andesite Differentiation: A Comprehensive Petrological and Geochemical Study of Arenal Volcano, Costa Rica
合作研究:调查安山岩分异的过程和时间尺度:哥斯达黎加阿雷纳尔火山的综合岩石学和地球化学研究
  • 批准号:
    0207761
  • 财政年份:
    2002
  • 资助金额:
    $ 6万
  • 项目类别:
    Standard Grant
Observational Constraints on Melt-Rock Reactions during Melting of the Upper Mantle
上地幔熔融过程中熔岩反应的观测限制
  • 批准号:
    0096533
  • 财政年份:
    2001
  • 资助金额:
    $ 6万
  • 项目类别:
    Continuing Grant

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