在东南太平洋上升下面的地幔不连续性结构从P-to-S转换了相
1Y. Shen, Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. A. F. Sheehan, K. G. Dueker, H. Gilbert, Cooperative Institute for Research in Environmental Sciences (CIRES), University of.
概括
地震接收器功能揭示了南太平洋东部上升下方的正常地幔过渡区厚度. 这表明那里的上游不涉及地幔过渡区的过度热量.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地球科学 地球科学 地球科学
背景情况:
- 地幔过渡区 (MTZ) 是理解地幔动态的一个关键区域.
- 海底地震计为地球深层结构的地震成像提供了关键数据.
研究的目的:
- 调查东南太平洋海拔下方的MTZ的结构和热状态.
- 为了确定地幔上升是否与异常的MTZ属性有关.
主要方法:
- 分析来自远震体波的接收器功能.
- 使用海底地震计记录地震数据.
- 识别地幔不连续性 (410公里和660公里深度) 的剪切波转换.
主要成果:
- 南部东太平洋上升下方的MTZ的厚度与全球平均值一致.
- 没有发现更浅或更厚的MTZ证据.
结论:
- 在东太平洋上升的南部下方的上升似乎与MTZ的过度温度无关.
- 这个区域下面的MTZ表现出正常的地震特性,表明没有显著的热异常.
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