Two models: global sea-level change and sequence stratigraphic architecture
- 31 December 1998
- journal article
- Published by Elsevier in Sedimentary Geology
- Vol. 122 (1-4) , 23-36
- https://doi.org/10.1016/s0037-0738(98)00111-0
Abstract
No abstract availableKeywords
This publication has 58 references indexed in Scilit:
- Stratigraphic modelling of epicontinental basins: two applicationsPublished by Elsevier ,2003
- Stranded parasequences and the forced regressive wedge systems tract: deposition during base-level fall—replyPublished by Elsevier ,2000
- Sequence concepts at seismic and outcrop scale: the distinction between physical and conceptual stratigraphic surfacesPublished by Elsevier ,1999
- Stratal Thickness Frequencies and the Prevalence of Orderedness in Stratigraphic SequencesThe Journal of Geology, 1996
- Stranded parasequences and the forced regressive wedge systems tract: deposition during base-level fall—discussionSedimentary Geology, 1995
- Stranded parasequences and the forced regressive wedge systems tract: deposition during base-level'fallSedimentary Geology, 1992
- Inferred glacio-eustatic control for high-frequency depositional sequences of the Plio-Pleistocene Kazusa Group, a forearc basin fill in Boso Peninsula, JapanSedimentary Geology, 1992
- High-frequency depositional sequences of the upper part of the Kazusa Group, a middle Pleistocene forearc basin fill in Boso Peninsula, JapanSedimentary Geology, 1992
- Pleistocene evolution: Northern hemisphere ice sheets and North Atlantic OceanPaleoceanography and Paleoclimatology, 1989
- Tectonic subsidence, flexure and global changes of sea levelNature, 1982