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- W2039684673 abstract "Abstract In the western Woodlark Basin within the neovolcanic zone sediments form ponds in fissures and between individual pillows and tubes. A continuous thin sediment cover appears only at the base of the neovolcanic zone. Its thickness increases with the distance from the zone. Data on the lithology, mineralogy and chemistry of sediment cores from the spreading centre in the western Woodlark Basin and adjacent areas show that these calcareous sediments (avg. 44.1 % CaCO 3 ) contain significant amounts of terrigenous, arc volcanic, hyaloclastic and hydrothermal material, the latter constituting up to 15% of the non-carbonate fraction. Two types of sedimentary sequences occur in the studied area. Those of the first type were formed by particle-by-particle sedimentation; horizons of redeposited sediments occur in sequences of the second type. Redeposition of sediments is widespread and is tentatively correlated with cycles of volcanic activity at swells along the spreading centre. These alternate with hydrothermal cycles, which were determined by the presence of hydrothermal matter in sediments. Radiocarbon dating of sediments showed that both cycles are of similar duration, of the order of 10,000 years. They are not synchronous along the spreading axis, each swell having a specific evolution. Based on these determinations we can say that within the studied spreading centre only the Franklin Seamount swell is prospective for contemporary hydrothermal activity." @default.
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- W2039684673 date "1997-10-01" @default.
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- W2039684673 title "Sediments of the active rift zone in the western Woodlark Basin and the development of hydrothermal and volcanic activity" @default.
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- W2039684673 doi "https://doi.org/10.1016/s0025-3227(97)00048-0" @default.
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