一个‘室内’地质学家的网络空间
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中文 (简体)
中文 (简体)
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Normal fault
Response of unconfined turbidity current to normal‐fault topography
We use numerical simulation to study reactions of turbidity current to typical half-graben scale normal faults in rift basins. We find the fault-related topography has a direct impact upon its flow behaviour and preferential area of deposition.
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