西藏东部地区层析成像及东南部裂谷成因讨论
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摘要
利用西藏东部南迦巴瓦地区的51个临时地震台站所记录的169个远震事件,从中提取出4767条P波射线,通过反演计算得到了西藏东部地壳和上地幔的P波速度结构.水平剖面显示,在西藏东南部裂谷附近从近地表到250km的深度范围均表现为低速异常;从纵剖面结果看,这个低速异常非垂直地向下延伸到约400km深度.综合分析认为,此低速异常可能意味着地幔高温物质上涌,从而为该区裂谷成因的探讨提供了地震学的证据;在此低速异常的东侧出现明显的高速异常,深度从40km延伸到200km,该高速异常可能是大陆闭合遗留的产物,并非俯冲的印度板块;在250~400km的深度范围内,嘉黎断裂以北为低速异常区,以南为高速异常区.该高速异常可能反映了印度板块的北部边界,并在此发生了拆沉.同时表明,在西藏东部印度板块的俯冲未超过嘉黎断裂.
引文
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