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High Pressure Single Crystal Diffraction at PX^2
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由于夏威夷羽毛,石质层的再生
Xueqing Li1, Rainer Kind, Xiaohui Yuan
1GeoForschungsZentrum Potsdam, Telegrafenberg, 14473 Potsdam, Germany.
Nature
|February 27, 2004
概括
夏威夷群岛是夏威夷群岛的一个组成部分.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 板块构造学是一种板块构造学.
背景情况:
- 夏威夷的火山活动与海洋石化层在固定地幔羽毛上的运动有关.
- 现有的地震成像缺乏分辨率,以区分羽毛-石质层相互作用模型.
研究的目的:
- 使用地震接收器功能绘制夏威夷群岛下方的石质层厚度图.
- 研究羽毛-石质层相互作用及其对岛屿链形成的影响.
主要方法:
- 应用S波接收器功能的技术.
- 来自夏威夷群岛三个永久宽带站的地震数据的分析.
主要成果:
- 大岛下方的石化层厚度为100-110公里,与未经修改的旧海洋板相一致.
- 石化层逐渐在卡瓦伊岛下面的50-60公里变薄,宽度超过300公里.
- 有证据表明,复苏模式在稀释区内是活跃的.
结论:
- 地幔羽毛积极稀释沿夏威夷岛屿链沿线的石化层.
- 更广泛的地形膨胀很可能是由动态力量支的,而不仅仅是石质层稀薄.
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