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The seismic reflection method has been used to map the thickness of sediments in many parts of the oceans.
The total thickness of sediments significantly affects the seismic response at longer periods around the fundamental period of the studied valley sections between 1.8 and 3.6 s.
Moreover, areas of gravity lows have greater thickness of sediments than areas of gravity highs.
These include the convergence rate, the thickness of sediments, seismicity, seismic coupling, and SSEs.
In the CRZ, the thickness of sediments is more than 1 m, making cultivation difficult.
Variable thickness of sediments is also apparent on the seaward horst compared to the graben at the trench axis.
Similar(48)
Generally, the thickness of sediment on the oceanic crust increases with the age of the crust.
These deposits are usually thin and maintain a constant thickness of sediment that rests on a flat surface eroded across the underlying bedrock or unconsolidated debris.
In the 1960s the Joint Oceanographic Institutions for Deep Earth Sampling deep-drilling project penetrated the entire thickness of sediment in the Atlantic.
Along the transect they measured topographic profile and thickness of sediment deposited by the 2004 tsunami.
The main result obtained from this study is the thickness of sediment cover.
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