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Heath, G Ross; Rea, David K; Levi, Shaul (1985): Paleomagnetism at DSDP Sites 86-576 and 86-578 [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.802301, Supplement to: Heath, GR et al. (1985): Paleomagnetism and accumulation rates of sediments at Sites 576 and 578, Deep Sea Drilling Project Leg 86, western North Pacific. In: Heath GR; Burckle LH; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 86, 459-502, https://doi.org/10.2973/dsdp.proc.86.118.1985

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Abstract:
The upper sections of Deep Sea Drilling Project Sites 576 (32°21.4'N, 164°16.5'E) and 578 (33°55.6'N, 151°37.7'E) both have stable detrital remanence that can be correlated with the standard reversal stratigraphy. Site 576 contains all reversals above the base of the Gilbert Epoch (5 m.y.) at about 25 m, whereas Site 578 contains a remarkable section of about 60 reversals extending to Anomaly 5B (15 m.y.) at about 150 m sub-bottom depth. In both cases, the paleomagnetic stratigraphy breaks down when accumulation rates drop below 2 m/m.y. At both sites, authigenic manganiferous clays deposited from 70 to 16 m.y. ago accumulated at about 0.4 m/m.y. Similarly, at both sites, the Pleistocene pulse of eolian debris increased accumulation rates by about 6 m/m.y.**2. From 16 to 2 m.y. ago, however, sediment accumulated at Site 578 about five times as rapidly as at Site 576, apparently because of augmented input to the western site by bottom currents.
Project(s):
Coverage:
Median Latitude: 32.944812 * Median Longitude: 159.533062 * South-bound Latitude: 32.356000 * West-bound Longitude: 151.629000 * North-bound Latitude: 33.926000 * East-bound Longitude: 164.275700
Date/Time Start: 1982-05-16T00:00:00 * Date/Time End: 1982-05-27T00:00:00
Size:
8 datasets

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