Abstract
The input of terrigenous sediment along the tectonically active Makran continental margin off south-western Pakistan (Gulf of Oman, northern Arabian Sea) is studied on the basis of sediment cores distributed along a transect from the upper slope to the abyssal plain. Spatial and temporal variations in sediment composition, sedimentation rate and turbidite frequency in late Pleistocene-Holocene time (last ~20
Original language | English |
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Pages (from-to) | 351-371 |
Journal | Marine Geology |
Volume | 169 |
Issue number | (3-4) |
DOIs | |
Publication status | Published - 2000 |