Marshall Paraconformity: a mid-Oligocene record of inception of the Antarctic circumpolar current and coeval glacio-eustatic lowstand?
- 1 February 1996
- journal article
- Published by Elsevier in Marine and Petroleum Geology
- Vol. 13 (1), 61-77
- https://doi.org/10.1016/0264-8172(95)00033-x
Abstract
No abstract availableThis publication has 36 references indexed in Scilit:
- Integrated Late Eocene‐Oligocene Stratigraphy of the Alabama Coastal Plain: Correlation of Hiatuses and Stratal Surfaces to Glacioeustatic LoweringsPaleoceanography and Paleoclimatology, 1993
- Miocene isotope reference section, Deep Sea Drilling Project Site 608: An evaluation of isotope and biostratigraphic resolutionPaleoceanography and Paleoclimatology, 1991
- Upper Eocene to Oligocene isotope (87Sr/86Sr, δ18O, δ13C) standard section, Deep Sea Drilling Project Site 522Paleoceanography and Paleoclimatology, 1988
- Mid-Tertiary unconformities in north Otago — A review and assessmentJournal of the Royal Society of New Zealand, 1988
- Mid-Tertiary unconformities in the Waitaki Subdivision, North Otago — a commentJournal of the Royal Society of New Zealand, 1987
- Oligo-Miocene unconformities in North Otago and the Tasman SeaJournal of the Royal Society of New Zealand, 1987
- The Motunau Fault and other structures at the southern edge of the Australian-Pacific plate boundary, offshore Marlborough, New ZealandTectonophysics, 1982
- The Marshall Paraconformity (Note)New Zealand Journal of Geology and Geophysics, 1980
- Cainozoic sedimentation in basins adjacent to a major continental transform boundary in southern New ZealandJournal of the Geological Society, 1978
- Paleoenvironmental implications of stormscoured, ichnofossiliferous mid-tertiary limestones, Waihao district, south Canterbury, New ZealandNew Zealand Journal of Geology and Geophysics, 1975