Detection of slow anomaly in the lower mantle beneath the Philippine Sea Plate from three-dimensiona

来源 :2014中国科学院计算地球动力学重点实验室国际学术研讨会暨实验室学术年会(2014计算地球动力学前沿问题国际学术研讨会暨 | 被引量 : 0次 | 上传用户：t60720372f

【摘要】

：

【作者】

：

CUI Hui-Hui ZHOU Yuan-Ze

【机构】

：

College of Earth Sciences,University of ChineseAcademy of Sciences,Beijing,100049

【出处】

：

2014中国科学院计算地球动力学重点实验室国际学术研讨会暨实验室学术年会(2014计算地球动力学前沿问题国际学术研讨会暨

【发表日期】

：

2014年11期

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The mantle plumes rising from different depths show seismic slow anomaly in deep Earth and could influence the process of the regional geodynamic evolution.Ocean island chains resulted from the moving plates on mantle plumes form long lines of volcanoes with progressively increasing ages(Hofmann,1997).

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Detection of slow anomaly in the lower mantle beneath the Philippine Sea Plate from three-dimensiona

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