Constraints on the timing of systems tract development with respect to sixth-order (41 ka) sea-level changes: an example from the Pleistocene Omma Formation, Sea of Japan

This publication has 15 references indexed in Scilit:

• Change in the thickness of the warm Tsushima Current at the initiation of its flow into the Sea of Japan
  Palaeogeography, Palaeoclimatology, Palaeoecology, 1999
• Sequence concepts at seismic and outcrop scale: the distinction between physical and conceptual stratigraphic surfaces
  Published by Elsevier ,1999
• The relationship between shellbed type and sequence architecture: examples from Japan and New Zealand
  Published by Elsevier ,1999
• Glaucony and carbonate grains as indicators of the condensed section: Omma Formation, Japan
  Sedimentary Geology, 1998
• Exposed coasts vs sheltered bays: contrast between New Zealand and Japan in the molluscan record of temperature change in Plio–Pleistocene cyclothems
  Sedimentary Geology, 1998
• Reconstruction of the thickness of the Tsushima current in the Sea of Japan during the Quaternary from molluscan fossils
  Palaeogeography, Palaeoclimatology, Palaeoecology, 1997
• Sequence stratigraphy of sixth-order (41 k.y.) Pliocene–Pleistocene cyclothems, Wanganui basin, New Zealand: A case for the regressive systems tract
  GSA Bulletin, 1997
• Cyclic changes in lithofacies and molluscan content in the early Pleistocene Omma Formation, Central Japan related to the 41,000-year orbital obliquity
  Palaeogeography, Palaeoclimatology, Palaeoecology, 1994
• Pleistocene evolution: Northern hemisphere ice sheets and North Atlantic Ocean
  Paleoceanography and Paleoclimatology, 1989
• Calcareous microfossil biostratigraphy of the uppermost cenozoic formations distributed in the coast of the Japan Sea. Part 2. Hokuriku Sedimentary Basin.
  Journal of the Japanese Association for Petroleum Technology, 1988