There are vast non-consolidated alluvia deposits freshly formed in estuary area of Yangtze River and nearby coastal area.The deposits contribute to land subsidence.
摘要长江河口滨海地区广泛分布有大量的填土,由于其形成时间短,具有欠固结特,因此对地面沉降影响较大。
There are vast non-consolidated alluvia deposits freshly formed in estuary area of Yangtze River and nearby coastal area.The deposits contribute to land subsidence.
摘要长江河口滨海地区广泛分布有大量的填土,由于其形成时间短,具有欠固结特,因此对地面沉降影响较大。
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