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(Table 1) Consolidation characteristics and physical properties for DSDP Legs...
Consolidation characteristics of marine sediments have been determined for several different geologic provinces (cf. Hamilton, 1959, 1964; Keller and Bennett, 1973; Trabant,... -
(Table 1) Lithology, mineralogy, and physical properties of Cretaceous cherts...
Cretaceous chert and porcellanite recovered at Site 436, east of northern Honshu, Japan, are texturally and mineralogically similar to siliceous rocks of comparable age at Sites... -
(Table 1) Heavy minerals at DSDP Legs 56-57 Holes
Heavy-mineral assemblages in the cored sediments from DSDP Legs 56 and 57 show a distinct change of source rocks, from older sedimentary rocks during the Oligocene to volcanic... -
(Table 1) Typical trace-fossil occurrences in DSDP Holes 56-436 and 56-435A
Trace fossils are in places abundant in cores from DSDP Leg 56 sites. They are particularly rich in the pelagic-clay sequence at Site 436. Some significant trace fossils,... -
(Table 1) Occurrence of ichthyoliths at DSDP Hole 56-436
Approximately 20 meters of the section near the bottom of Hole 436 was "unfossiliferous," overlain by middle Miocene mudstone with siliceous microfossils and underlain by...
