Browsing by Author "Naish, Timothy R."
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An integrated sequence stratigraphic, palaeoenvironmental, and chronostratigraphic analysis of the Tangahoe Formation, southern Taranaki coast, with implications for mid-Pliocene (c. 3.4–3.0 Ma) glacio-eustatic sea-level changes
Naish, Timothy R.; Wehland, Florian; Wilson, Gary S.; Browne, Gregory H.; Cook, Richard A.; Morgans, Hugh E.G.; Rosenberg, Michael; King, Peter R.; Smale, David; Nelson, Campbell S.; Kamp, Peter J.J.; Richetts, Brian (SIR Publishing, 2005)Sediments of the mid-Pliocene (c. 3.4–3.0 Ma) Tangahoe Formation exposed in cliffs along the South Taranaki coastline of New Zealand comprise a 270 m thick, cyclothemic shallow-marine succession that has been gently warped ... -
Late Holocene mud sedimentation and diagenesis in the Firth of Thames: Bentonites in the making
Naish, Timothy R. (University of Waikato, 1990)Late Holocene mud sedimentation in the southern Firth of Thames has been described from analysis of a number of shallow marine sediment cores. Three distinct lithofacies are distinguished on the basis of sediment texture ... -
Megasequence architecture of Taranaki, Wanganui, and King Country basins and Neogene progradation of two continental margin wedges across western New Zealand.
Kamp, Peter J.J.; Vonk, Adam J.; Bland, Kyle J.; Griffin, Angela.G.; Hayton, Shaun; Hendy, Austin J.W.; McIntyre, Avon P.; Nelson, Campbell S.; Naish, Timothy R. (Crown Minerals, Ministry of Economic Development, 2002)Taranaki, Wanganui and King Country basins (formerly North Wanganui Basin) have been regarded as discrete basins, but they contain a very similar Neogene sedimentary succession and much of their geological history is held ... -
Pliocene-Pleistocene marine cyclothems, Wanganui Basin, New Zealand: a lithostratigraphic framework
Naish, Timothy R.; Kamp, Peter J.J. (The Royal Society of New Zealand, 1995)The Rangitikei River valley between Mangaweka and Vinegar Hill and the surrounding Ohingaiti region in eastern Wanganui Basin contains a late Pliocene to early Pleistocene (c. 2.6-1.7 Ma), c. 1100 m thick, southward-dipping ... -
Towards an understanding of thermodynamic and kinetic controls on the formation of clay minerals from volcanic glass under various environmental conditions
Hodder, A.P.W.; Naish, Timothy R.; Lowe, David J. (Research Signpost, 1996-01-01)lmogolite is the kinetically and thermodynamically favoured weathering product from rhyolitic volcanic glass in the soil-forming environment. However, on thermodynamic grounds imogolite would also appear to be the favoured ...
Co-authors for Timothy R. Naish
Timothy R. Naish has 19 co-authors in Research Commons.