Stratal architecture of Western Mediterranean Margins as the result of the stacking of Quaternary lowstand deposits below ‘glacio-eustatic fluctuation base-level’
- 1 September 1997
- journal article
- Published by Elsevier in Sedimentary Geology
- Vol. 112 (3-4) , 195-217
- https://doi.org/10.1016/s0037-0738(97)00035-3
Abstract
No abstract availableKeywords
This publication has 32 references indexed in Scilit:
- Lowstand terraces on Tyrrhenian Sea steep continental slopesMarine Geology, 1996
- Pleistocene progradational growth pattern of the northern Catalonia continental shelf (northwestern Mediterranean)Geo-Marine Letters, 1994
- Late Quaternary transgressive erosion and deposition in a modern epicontinental shelf: The Adriatic semienclosed basinGeo-Marine Letters, 1994
- Neogene tectonic evolution of the Alboran Sea from MCS dataGeo-Marine Letters, 1992
- Sedimentary evolution of the northwestern Alboran Sea during the QuaternaryGeo-Marine Letters, 1992
- Deep crustal configuration of the Valencia trough and its Iberian and Balearic borders from extensive refraction and wide-angle reflection seismic profilingTectonophysics, 1992
- Late Quaternary deltaic lowstand wedges on the Rhône continental shelf, FranceMarine Geology, 1990
- Relation of sequence stratigraphy to modern sedimentary environmentsGeology, 1989
- ODP Leg 107 in the Tyrrhenian Sea: Insights into passive margin and back-arc basin evolutionGSA Bulletin, 1988
- Global Maps of Lake-Level Fluctuations since 30,000 yr B.P.Quaternary Research, 1979