The architectural variability of small-scale cycles in shelf and ramp clastic systems: The controlling factors
- 1 September 2007
- journal article
- Published by Elsevier in Earth-Science Reviews
- Vol. 84 (1-2) , 21-55
Abstract
No abstract availableKeywords
This publication has 92 references indexed in Scilit:
- Orbital forcing recorded in subtidal cycles from a Lower Miocene siliciclastic–carbonate ramp system (Central Italy)Terra Nova, 2005
- Stratigraphy and sedimentology of fault-controlled backstepping shorefaces, middle Pliocene of Crotone Basin, Southern ItalySedimentary Geology, 2005
- Raised Pleistocene marine terraces of the Crotone peninsula (Calabria, southern Italy): facies analysis and organization of their depositsSedimentary Geology, 2004
- Numerical modelling of depositional sequences in half‐graben rift basinsSedimentology, 2003
- Predicting the pinchout distance of shoreline tonguesTerra Nova, 2001
- Anatomy of high-sediment supply, transgressive tracts in the Vilomara composite sequence, Sant Llorenç del Munt, Ebro Basin, NE SpainSedimentary Geology, 2000
- Unusual features of sediment supply-dominated, transgressive–regressive sequences: Paleogene clastic wedges, SE Pyrenean foreland basin, SpainSedimentary Geology, 2000
- Architecture of the tectonically influenced Sobrarbe deltaic complex in the Ainsa Basin, northern SpainSedimentary Geology, 1999
- Forward modelling of the sequence stratigraphic architecture of shelf cyclothems: application to Late Pliocene sequences, Wanganui Basin (New Zealand)Sedimentary Geology, 1998
- Stranded parasequences and the forced regressive wedge systems tract: deposition during base-level'fallSedimentary Geology, 1992