Lyle, Mitchell W; Owen, Robert M; Leinen, Margaret W (1986): Mass accumulation rates, age, sedimentation rate and bulk density at the East Pacific Rise. PANGAEA, https://doi.org/10.1594/PANGAEA.792731, Supplement to: Lyle, MW et al. (1986): History of hydrothermal sedimentation at the East Pacific Rise, 19°S. In: Leinen, M; Rea DK; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 92, 585-596, https://doi.org/10.2973/dsdp.proc.92.139.1986
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The rate at which hydrothermal precipitates accumulate, as measured by the accumulation rate of manganese, can be used to identify periods of anomalous hydrothermal activity in the past. From a preliminary study of Sites 597 and 598, four periods prior to 6 Ma of anomalously high hydrothermal activity have been identified: 8.5 to 10.5 Ma, 12 to 16 Ma, 17 to 18 Ma, and 23-to-27 Ma. The 18-Ma anomaly is the largest and is associated with the jump in spreading from the fossil Mendoza Ridge to the East Pacific Rise, whereas the 23-to-27-Ma anomaly is correlated with the birth of the Galapagos Spreading Center and resultant ridge reorganization. The 12-to-16-Ma and 8.5-to-10.5-Ma anomalies are correlated with periods of anomalously high volcanism around the rim of the Pacific Basin and may be related to other periods of ridge reorganization along the East Pacific Rise. There is no apparent correlation between periods of fast spreading at 19°S and periods of high hydrothermal activity. We thus suggest that periods when hydrothermal activity and crustal alteration at mid-ocean ridges are the most pronounced may be periods of large-scale ridge reorganization.
Median Latitude: -18.612562 * Median Longitude: -120.862347 * South-bound Latitude: -20.000000 * West-bound Longitude: -129.770500 * North-bound Latitude: -16.930000 * East-bound Longitude: -113.500000
Date/Time Start: 1963-04-24T00:00:00 * Date/Time End: 1983-03-25T00:00:00