Transgressive systems tracts and onlap shellbeds from mid-pleistocene sequences, wanganui basin, New Zealand

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Department of Earth Sciences, James Cook University of North Queensland, QLD 4811, Australia ^{[1
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J. Sediment. Res. | / 2卷 / 253-268期

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[31] Sequence stratigraphy of sixth-order (41 ky) Pliocene-Pleistocene cyclothems, Wanganui basin, New Zealand: A case for the regressive systems tract
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[32] MAGNETOSTRATIGRAPHIC, LITHOSTRATIGRAPHIC AND TEPHROSTRATIGRAPHIC CONSTRAINTS ON LOWER AND MIDDLE PLEISTOCENE SEA-LEVEL CHANGES, WANGANUI BASIN, NEW-ZEALAND
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[33] Forward modelling of the sequence stratigraphic architecture of shelf cyclothems: application to Late Pliocene sequences, Wanganui Basin (New Zealand)
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[34] 10Be spikes in Plio-Pleistocene cyclothems, Wanganui Basin, New Zealand:: identification of the local flooding surface (LFS)
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[36] Forward modelling of the sequence stratigraphic architecture of shelf cyclothems: application to Late Pliocene sequences, Wanganui Basin (New Zealand)
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[37] PALYNOLOGICAL EVIDENCE FOR UPPER PUTIKIAN (MIDDLE PLEISTOCENE) INTERGLACIAL AND GLACIAL CLIMATES AT RANGITAWA STREAM, SOUTH WANGANUI BASIN, NEW-ZEALAND
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[38] Sedimentary cyclicity in the marine Pliocene-Pleistocene of the Wanganui basin (New Zealand): Sequence stratigraphic motifs characteristic of the past 2.5 my
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[39] The stratigraphic architecture of Late Pliocene (2.8-2.4 Ma) asymmetrical shelf sequences, western Wanganui Basin, New Zealand
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[40] Sequence stratigraphy of sixth-order (41 k.y.) Pliocene-Pleistocene cyclothems, Wanganui basin, New Zealand: A case for the regressive systems tract
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