Deep earthquakes and the thermal assimilation of subducting lithosphere

作者: Rinus Wortel

DOI: 10.1029/GL013I001P00034

关键词:

摘要: Two problematic aspects of deep seismic zones are investigated: the maximum depth (about 700 km) activity and relative in energy release 500-700 km range. It is shown that both features can be accounted for by a model based on thermal assimilation. This implies no barrier required at 650-700 to explain observations.

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