The stratigraphic architecture of three adjacent valley bodies of post-LGM age buried beneath the northern coast of Tuscany is illustrated in detail. Above a gravel fluvial deposit, the valley fills exhibit a distinctive succession of coastal plain to estuarine facies, punctuated by an aggradational stacking pattern of millennial-scale depositional cycles with distinctive climatic signature. Radiocarbon dates document that the three valleys were active simultaneously and that rapidly created accommodation during transgression was filled under conditions of very high sediment supply
ABSTRACT: Incised valleys entirely filled with fluvial deposits are rarely described in the literatu...
Integrated sedimentological and micropalaeontological analysis of a 105 m long core (Vignarca) from ...
Palaeovalley systems developed during the last glacial-interglacial cycle and now buried beneath mod...
The stratigraphic architecture of three adjacent valley bodies of post-LGM age buried beneath the no...
Three prominent incised-valley fills of post-Last Glacial Maximum age are described from the norther...
Three consecutive, time-equivalent valley fills of Lateglacial-Holocene age (13 to 8 cal kyr BP) wer...
The Late Quaternary succession of the Italian Tyrrhenian coast contains several paleovalleys, formed...
Based on integrated sedimentological, micropaleontological (benthic foraminifers, ostracods) and chr...
Despite recent report of millennial-scale cyclicity from Lateglacial-Holocene deposits of severa! co...
The Ombrone palaeovalley was incised during the last glacial sea-level fall and was infilled during ...
"The late Quaternary Arno valley fill, in western Tuscany, was formed during the last glacio-eustati...
The Ombrone palaeovalley was incised during the last glacial sea-level fall and was infilled during ...
Downcutting and infill of incised valley systems is mostly controlled by relative sea-level changes,...
Despite the worldwide report of high-frequency depositiana! cycles from the Lateglacial-Holocene sub...
none4noUn-fragmented stratigraphic records of late Quaternary multiple incised valley systems are ra...
ABSTRACT: Incised valleys entirely filled with fluvial deposits are rarely described in the literatu...
Integrated sedimentological and micropalaeontological analysis of a 105 m long core (Vignarca) from ...
Palaeovalley systems developed during the last glacial-interglacial cycle and now buried beneath mod...
The stratigraphic architecture of three adjacent valley bodies of post-LGM age buried beneath the no...
Three prominent incised-valley fills of post-Last Glacial Maximum age are described from the norther...
Three consecutive, time-equivalent valley fills of Lateglacial-Holocene age (13 to 8 cal kyr BP) wer...
The Late Quaternary succession of the Italian Tyrrhenian coast contains several paleovalleys, formed...
Based on integrated sedimentological, micropaleontological (benthic foraminifers, ostracods) and chr...
Despite recent report of millennial-scale cyclicity from Lateglacial-Holocene deposits of severa! co...
The Ombrone palaeovalley was incised during the last glacial sea-level fall and was infilled during ...
"The late Quaternary Arno valley fill, in western Tuscany, was formed during the last glacio-eustati...
The Ombrone palaeovalley was incised during the last glacial sea-level fall and was infilled during ...
Downcutting and infill of incised valley systems is mostly controlled by relative sea-level changes,...
Despite the worldwide report of high-frequency depositiana! cycles from the Lateglacial-Holocene sub...
none4noUn-fragmented stratigraphic records of late Quaternary multiple incised valley systems are ra...
ABSTRACT: Incised valleys entirely filled with fluvial deposits are rarely described in the literatu...
Integrated sedimentological and micropalaeontological analysis of a 105 m long core (Vignarca) from ...
Palaeovalley systems developed during the last glacial-interglacial cycle and now buried beneath mod...