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Fluid-Assisted Deformation and Strain Localization in the Cooling Mantle Wedge of a Young Subduction Zone (Semail Ophiolite)

机译：幼眼区的冷却罩楔下的流体辅助变形和应变定位（糖矿石氨矿）

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C. Prigent; S. Guillot; P. Agard; B. Ildefonse;
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1. Fluid‐Assisted Deformation and Strain Localization in the Cooling Mantle Wedge of a Young Subduction Zone (Semail Ophiolite) [J] . Prigent C., Guillot S., Agard P., Journal of geophysical research. Solid earth: JGR . 2018,第9期

机译：在幼郊区（糖氨矿）的冷却罩楔下的流体辅助变形和应变定位
2. Transfer of subduction fluids into the deforming mantle wedge during nascent subduction: Evidence from trace elements and boron isotopes (Semail ophiolite, Oman) [J] . C. Prigent, S. Guillot, P. Agard, Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System . 2018,第期

机译：将俯冲流体转移到新生俯冲期间的变形搭扣楔数：来自微量元素和硼同位素的证据（糖矿石，阿曼）
3. Strain localization and fluid infiltration in the mantle wedge during subduction initiation: Evidence from the base of the New Caledonia ophiolite [J] . Soret M., Agard P., Dubacq B., Lithos: An International Journal of Mineralogy, Petrology, and Geochemistry . 2016,第Null期

机译：俯冲开始期间地幔楔中的应变局部化和流体渗透：来自新喀里多尼亚蛇绿岩底部的证据
4. Deformation patterns of an accretionary wedge in the transition zone from subduction to collision offshore southwestern Taiwan [C] . Char-Shine Liu, Deffontaines, B., . 2003

机译：从俯冲到碰撞的过渡带中增生楔的变形模式
5. Seismic anisotropy, lithospheric deformation, and mantle flow in subduction zones, continental keels, and the core-mantle boundary. [D] . Fouch, Matthew James. 1999

机译：俯冲带，大陆龙骨和岩心—地幔边界的地震各向异性，岩石圈变形和地幔流动。
6. Seismic evidence for flow in the hydrated mantle wedge of the Ryukyu subduction zone [O] . Takayoshi Nagaya, Andrew M. Walker, James Wookey, -1

机译：琉球俯冲带水合地幔楔中流动的地震证据
7. Strain localization and fluid infiltration in the mantle wedge during subduction initiation: Evidence from the base of the New Caledonia ophiolite [O] . Soret Mathieu, Agard Philippe, Dubacq Benoît, 2016

机译：俯冲开始期间地幔楔中的应变局部化和流体渗透：来自新喀里多尼亚蛇绿岩底部的证据

Fluid-Assisted Deformation and Strain Localization in the Cooling Mantle Wedge of a Young Subduction Zone (Semail Ophiolite)

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