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首页> 外文期刊>Geophysical Research Letters >Reply to 'Comment on 'A new estimate for present-day Cocos-Caribbean plate motion: Implications for slip along the central American volcanic arc'' by Marco Guzman-Speziale and Juan Martin Gomez - art. no. 1946
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Reply to 'Comment on 'A new estimate for present-day Cocos-Caribbean plate motion: Implications for slip along the central American volcanic arc'' by Marco Guzman-Speziale and Juan Martin Gomez - art. no. 1946

机译:Marco Guzman-Speziale和Juan Martin Gomez对艺术界的答复:“对'对当今科科斯-加勒比板块运动的新估计:对沿着美国中部火山弧滑动的影响的评论'的评论”。没有。 1946年

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I thank Guzman-Speziale and Gomez (GSG02) for their comments on DeMets (2001) (DM2001). GSG02 do not challenge the fundamental observation reported by DM2001, namely, that earthquake slip directions along the Middle America trench between western Guatemala and Costa Rica are rotated similar to10degrees clockwise relative to the Cocos-Caribbean convergence direction. However, they dispute the interpretation that this oblique convergence causes dextral shear across the Central American forearc in this region [White, 1991; DeMets, 2001]. Below, I address their reservations. [References: 11]
机译:感谢Guzman-Speziale和Gomez(GSG02)对DeMets(2001)(DM2001)的评论。 GSG02不会挑战DM2001报道的基本观察,即,沿危地马拉西部和哥斯达黎加之间的中美洲海沟的地震滑动方向相对于Cocos-Caribbean收敛方向沿顺时针方向旋转了10度。然而,他们对这种倾斜的汇聚作用在该地区的中美洲前臂造成右旋剪切的解释提出了质疑[White,1991; DeMets,2001年]。下面,我解决他们的保留意见。 [参考:11]

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