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2 Physical Properties of Marine Sediments - Blogs Unpad

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2<strong>Physical</strong> <strong>Properties</strong> <strong>of</strong> <strong>Marine</strong> <strong>Sediments</strong>Fig. 2.25 c, d Parasound Seismogram sections representing typical deep sea clay (Weddell Sea) and terrigenoussediments (Bengal Fan). Lengths and heights <strong>of</strong> both pr<strong>of</strong>iles amount to 50 km and 300 m, respectively. Verticalexaggeration (VE) is 111. The Parasound seismogram section from the Weddell Sea was kindly provided by G. Kuhn,Alfred-Wegener-Institute for Polar- and <strong>Marine</strong> Research, Bremerhaven, Germany and is an unpublished data setrecorded during RV Polarstern cruise ANT IX/4. Modified after Breitzke (1997).66

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