作者: Harold Leah , Åke Fagereng , Francesca Meneghini , Julia K. Morgan , Heather M. Savage
DOI: 10.1029/2019TC005965
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摘要: Calcareous‐pelagic input sediments are present at several subduction zones and deform differently to their siliciclastic counterparts. We investigate deformation in calcareous …