Shear Deformation of Upper Mantle Minerals: The Role of Water, Dynamic Recrystallization and Deformation

上地幔矿物的剪切变形:水的作用、动态重结晶和变形

基本信息

  • 批准号:
    9706329
  • 负责人:
  • 金额:
    $ 19.07万
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Continuing Grant
  • 财政年份:
    1997
  • 资助国家:
    美国
  • 起止时间:
    1997-09-01 至 1999-08-31
  • 项目状态:
    已结题

项目摘要

9706329 Karato The PI proposes to provide new experimental constraints on the geodynamical interpretation of seismic anisotropy in upper mantle minerals. The focus will be on the role of water and of dynamic recrystallization. Simple shear deformation techniques developed in the PI's laboratory will be used in the experiments and electron backscatter pattern analysis (EBSP) will be utilized to investigate lattice preferred orientation. Synthetic polycrystalline specimens of upper mantle minerals will be prepared and deformed to large strains (~100-300 %) at high temperature and pressure in simple shear under water-rich and water-poor conditions. The microstructural development including the lattice preferred orientation will be investigated by the EBSP technique and seismic anisotropy corresponding to specific deformation mechanisms and deformation geometry will be predicted. The results will be compared with seismological observations to place new constraints on the flow pattern in the upper mantle. ***
小行星9706329 PI建议为上地幔矿物中地震各向异性的地球动力学解释提供新的实验约束。 重点将放在水和动态重结晶的作用。 PI实验室开发的简单剪切变形技术将用于实验,电子背散射图案分析(EBSP)将用于研究晶格择优取向。 将制备上地幔矿物的合成多晶样品,并在高温高压下在富水和贫水条件下在简单剪切中变形至大应变(~100- 300%)。 将通过EBSP技术研究包括晶格择优取向在内的微结构发展,并预测对应于特定变形机制和变形几何形状的地震各向异性。 研究结果将与地震学观测结果进行比较,从而对上地幔的流动模式提出新的限制。 ***

项目成果

期刊论文数量(0)
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Shun-ichiro Karato其他文献

Properties and dynamics of mantle and core
地幔和地核的性质和动力学
  • DOI:
  • 发表时间:
    2008
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Bernhard Steinberger;Eiji Ohta ni;Geld Steinle-Neumann;Jame s Connolly;Shun-ichiro Karato
  • 通讯作者:
    Shun-ichiro Karato
High-resolution mapping of North America suggests numerous low-velocity zones above and below the mantle transition zone
对北美洲的高分辨率测绘显示,在地幔过渡带上下存在众多低速带。
  • DOI:
    10.1016/j.tecto.2025.230775
  • 发表时间:
    2025-06-27
  • 期刊:
  • 影响因子:
    2.600
  • 作者:
    Steve A.B. Carr;Tolulope Olugboji;Jeffrey Park;Shun-ichiro Karato
  • 通讯作者:
    Shun-ichiro Karato
Correction to: strength of single-crystal orthopyroxene under lithospheric conditions
  • DOI:
    10.1007/s00410-018-1458-1
  • 发表时间:
    2018-04-01
  • 期刊:
  • 影响因子:
    3.700
  • 作者:
    Tomohiro Ohuchi;Shun-ichiro Karato;Kiyoshi Fujino
  • 通讯作者:
    Kiyoshi Fujino
Pervasive low-velocity layer atop the 410-km discontinuity beneath the northwest Pacific subduction zone: Implications for rheology and geodynamics
  • DOI:
    https://doi.org/10.1016/j.epsl.2020.116642
  • 发表时间:
    2021
  • 期刊:
  • 影响因子:
  • 作者:
    Han Guangjie;Li Juan;Guo Guangrui;Walter D. Mooney;Shun-ichiro Karato;David A. Yuen
  • 通讯作者:
    David A. Yuen
Deep mantle melting, global water circulation and its implications for the stability of the ocean mass
  • DOI:
    10.1186/s40645-020-00379-3
  • 发表时间:
    2020-12-10
  • 期刊:
  • 影响因子:
    2.800
  • 作者:
    Shun-ichiro Karato;Bijaya Karki;Jeffrey Park
  • 通讯作者:
    Jeffrey Park

Shun-ichiro Karato的其他文献

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{{ truncateString('Shun-ichiro Karato', 18)}}的其他基金

Collaborative Research: CSEDI: Understanding the Role of Hydrogen and Melting in the Water Transport Across the Transition Zone-Lower Mantle Boundary
合作研究:CSEDI:了解氢和熔化在跨过渡带-下地幔边界的水传输中的作用
  • 批准号:
    2001339
  • 财政年份:
    2020
  • 资助金额:
    $ 19.07万
  • 项目类别:
    Standard Grant
Collaborative Research: Understanding the Origin of the mid-lithospheric discontinuity within a stable continent from a combined geophysics-mineral physics approach
合作研究:通过地球物理学-矿物物理学相结合的方法了解稳定大陆内岩石圈中部不连续性的起源
  • 批准号:
    1818792
  • 财政年份:
    2018
  • 资助金额:
    $ 19.07万
  • 项目类别:
    Standard Grant
CSEDI Collaborative Research: Understanding the nature of water transport between the transition zone and the lower mantle through the interdisciplinary studies
CSEDI合作研究:通过跨学科研究了解过渡带与下地幔之间的水运移本质
  • 批准号:
    1764271
  • 财政年份:
    2018
  • 资助金额:
    $ 19.07万
  • 项目类别:
    Continuing Grant
An experimental study on grain-size evolution during phase transformations in the mantle transition zone and its influence on rheological properties
地幔过渡带相变过程中晶粒尺寸演化及其对流变特性影响的实验研究
  • 批准号:
    1445356
  • 财政年份:
    2015
  • 资助金额:
    $ 19.07万
  • 项目类别:
    Continuing Grant
Experimental studies on plastic deformation of the lower mantle materials
下地幔材料塑性变形的实验研究
  • 批准号:
    1520006
  • 财政年份:
    2015
  • 资助金额:
    $ 19.07万
  • 项目类别:
    Continuing Grant
CSEDI Collaborative Research: Understanding the nature of water and melt transport between the transition zone and the lower mantle combining mineral physics and seismology
CSEDI合作研究:结合矿物物理和地震学了解过渡带和下地幔之间水和熔体传输的性质
  • 批准号:
    1464003
  • 财政年份:
    2015
  • 资助金额:
    $ 19.07万
  • 项目类别:
    Standard Grant
CSEDI Collaborative Research: Grand Challenge for Experimental Study of Plastic Deformation Under Deep Earth Conditions
CSEDI合作研究:深地条件下塑性变形实验研究的巨大挑战
  • 批准号:
    1361327
  • 财政年份:
    2014
  • 资助金额:
    $ 19.07万
  • 项目类别:
    Continuing Grant
CSEDI: Understanding the structure of the continental upper mantle through the use of magnetotelluric and seismic observations
CSEDI:通过使用大地电磁和地震观测了解大陆上地幔的结构
  • 批准号:
    1160932
  • 财政年份:
    2012
  • 资助金额:
    $ 19.07万
  • 项目类别:
    Standard Grant
An Experimental Study on the Strength of the Lithosphere: Large-strain shear deformation experiments of olivine + orthopyroxene aggregates
岩石圈强度的实验研究:橄榄石斜方辉石聚集体大应变剪切变形实验
  • 批准号:
    1214861
  • 财政年份:
    2012
  • 资助金额:
    $ 19.07万
  • 项目类别:
    Standard Grant
Experimental studies on rheological properties of transition zone minerals
过渡带矿物流变特性的实验研究
  • 批准号:
    1015336
  • 财政年份:
    2011
  • 资助金额:
    $ 19.07万
  • 项目类别:
    Continuing Grant

相似海外基金

Synchrotron deformation experiments of olivine under the deep upper mantle conditions: Transient creep, plastic anisotropy, and the role of grain-boundary sliding.
上地幔深部条件下橄榄石的同步加速变形实验:瞬态蠕变、塑性各向异性和晶界滑动的作用。
  • 批准号:
    2322719
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    2023
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Understanding the deformation and processes that link ductile flow in the deep continental crust with frictional processes in the upper crustal seismogenic zone
了解将深部大陆地壳中的延性流与上地壳地震带中的摩擦过程联系起来的变形和过程
  • 批准号:
    RGPIN-2020-05658
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    2022
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    Discovery Grants Program - Individual
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了解将深部大陆地壳中的延性流与上地壳地震带中的摩擦过程联系起来的变形和过程
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Transient rheology of upper mantle inferred from the postseismic deformation of 2011 Tohoku-oki earthquake
从2011年东北大地震震后形变推断的上地幔瞬态流变学
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  • 财政年份:
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温哥华岛南部上地壳的活跃变形
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  • 资助金额:
    $ 19.07万
  • 项目类别:
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