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- W2020937036 abstract "Abstract Since the late Oligocene ‐ early Miocene, three distinct uplift events have resulted in widespread sediment deposition in Central Otago, South Island, New Zealand. These events are marked in the sedimentary record by the early‐middle Miocene Manuherikia Group, late Miocene‐Pliocene Wedderburn and Maori Bottom Formations, and Quaternary schistose fan gravels. Each event was accompanied by some basement erosion and extensive recycling of older sediments. Early‐middle Miocene Manuherikia Group quartzose sands and conglomerates (Dunstan Formation) lying on the schist probably represent recycled early Tertiary freshwater ± marine sediments, still preserved in east and west Otago. Dunstan Formation sediments are cemented with framboidal marcasite and subordinate crystalline pyrite (both FeS2) to within a few metres of the surface at many localities. Heavy‐mineral concentrates from Quaternary alluvial fan sediments commonly contain small cubes and/or dodeca‐hedra of authigenic pyrite. Sand and conglomer..." @default.
- W2020937036 created "2016-06-24" @default.
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- W2020937036 date "1995-09-01" @default.
- W2020937036 modified "2023-09-26" @default.
- W2020937036 title "Sulphur mobility and sulphur‐mineral precipitation during early Miocene‐Recent uplift and sedimentation in Central Otago, New Zealand" @default.
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