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- W222742616 abstract "Middle Miocene to Holocene fine-grained argillaceous sediments (clays, claystones/muds, and mudstones), which volumetrically dominated the sediment recovery in the Woodlark Basin during Leg 180, were chemically analyzed for major elements, trace elements, and some rare earth elements by X-ray fluorescence. Selected samples also underwent X-ray diffraction (XRD) analysis for mineral determination. The results shed light on sediment provenance when combined with shipboard sediment descriptions, smear slide study, and XRD. The oldest sediments recovered (Site 1108) of middle–late Miocene age include volcanogenic muds with distinctive high MgO and K2O, indicative of a relatively basic calc-alkaline source related to an inferred Miocene forearc succession. The forearc basement, composed of diabase and basalt, was locally exposed (Site 1109) and eroded in the late Miocene ( [Cited YYYYMM-DD] 2Department of Geology and Geophysics, West Mains Road, University of Edinburgh, EH9 3JW, United Kingdom. ahfr@ginger.glg.ed.ac.uk 3University of Technology, Sydney, P.O. Box 123, Broadway, Sydney 2007, NSW, Australia. Initial receipt: 19 December 2000 Acceptance: 16 October 2001 Web publication: 12 March 2002" @default.
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- W222742616 date "2002-03-12" @default.
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- W222742616 title "Geochemical and mineralogical evidence for the provenance of mixed volcanogenic/terrigenous hemipelagic sediments in the Pliocene–Pleistocene Woodlark backarc rift basin, southwest Pacific: Ocean Drilling Program Leg 180" @default.
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- W222742616 doi "https://doi.org/10.2973/odp.proc.sr.180.156.2002" @default.
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