A review of Wanganui Basin, New Zealand: global reference section for shallow marine, Plio–Pleistocene (2.5–0 Ma) cyclostratigraphy
Author:
Publisher
Elsevier BV
Subject
Stratigraphy,Geology
Reference122 articles.
1. Relocation of the mid-Pleistocene Waiomio Shellbed (Putikian, c. 500 ka), and definition of the Waiomio Formation, Rangitikei Valley, Wanganui Basin;Abbott;Alcheringa,1992
2. Foraminiferal paleobathymetry and mid-cycle architecture of mid-Pleistocene depositional sequences, Wanganui Basin, New Zealand;Abbott;Palaios,1997
3. Mid-cycle condensed shellbeds from mid-Pleistocene cyclothems, New Zealand: implications for sequence architecture;Abbott;Sedimentology,1997
4. Abbott, S.T., 1998. Transgressive systems tracts and onlap shellbeds from mid-Pleistocene sequences, Wanganui Basin, New Zealand. J. Sediment. Res., in press.
5. Abbott, S.T., Carter, R.M., 1994. The sequence architecture of mid-Pleistocene (0.35–0.95 Ma) cyclothems from New Zealand: facies development during a period of known orbital control on sea-level cyclicity. In: De Boer, P.L., Smith, D.G. (Eds.), Orbital Forcing and Cyclic Sequences. Int. Assoc. Sedimentol. Spec. Publ. 19, 367–394.
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