Low-Velocity Structure of Subducted Oceanic Crust in the Upper Mantle: Insights from High Pressure and Temperature Elasticity Measurements of Aragonite
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Low-Velocity Structure of Subducted Oceanic Crust in the Upper Mantle: Insights from High Pressure and Temperature Elasticity Measurements of Aragonite.
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Zenodo创建时间：
2023-04-13
