2007
DOI: 10.2110/jsr.2007.030
|View full text |Cite
|
Sign up to set email alerts
|

Superimposed Cycles of Composite Marine Terraces: The Example of Cutro Terrace (Calabria, Southern Italy)

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

3
31
0

Year Published

2009
2009
2022
2022

Publication Types

Select...
7
1

Relationship

0
8

Authors

Journals

citations
Cited by 31 publications
(34 citation statements)
references
References 36 publications
3
31
0
Order By: Relevance
“…These resemble the internal arrangement of composite terraces resulting from the interplay between crustal uplift and successive transgressions during a composite interglacial stage. An example is the Cutro composite terrace reported by Nalin et al (2007), which is interpreted as the result of the reiteration of three transgressions of the same amplitude during the interglacial MIS 7, acting on a rising landmass. The attached terrace successions in the study area were not generated by slower crustal uplift than the detached successions, because both occur within comparable elevation ranges.…”
Section: Influence Of Long-term Upliftmentioning
confidence: 99%
See 1 more Smart Citation
“…These resemble the internal arrangement of composite terraces resulting from the interplay between crustal uplift and successive transgressions during a composite interglacial stage. An example is the Cutro composite terrace reported by Nalin et al (2007), which is interpreted as the result of the reiteration of three transgressions of the same amplitude during the interglacial MIS 7, acting on a rising landmass. The attached terrace successions in the study area were not generated by slower crustal uplift than the detached successions, because both occur within comparable elevation ranges.…”
Section: Influence Of Long-term Upliftmentioning
confidence: 99%
“…Interpretation -This lithofacies reflects accretion of a beach sand body during progradation in an upper shoreface depositional environment (Walker and Plint, 1992;Hart and Plint, 1995;Reading and Collison, 1996;Massari and Parea, 1988;Nalin et al, 2007). Deposition of sands mainly occurs under the action of strong seaward directed currents, as indicated by prevalent foreset orientation normal to present shoreline.…”
Section: Lithofacies A5 -Cross-stratified Sandsmentioning
confidence: 99%
“…The ca. 100 m-scale glacio-eustatic changes related to the 100 kyr eccentricity cycle, accompanied by lower-rank sea-level variations related to the obliquity-and precession-driven periodicities, were concomitant with the uplift of Calabria since latest early Pleistocene, producing flights of marine terraces along both the Ionian and Tyrrhenian coasts (Dumas et al, 1982;Gliozzi, 1987;Carobene and Dai Pra, 1990;Miyauchi et al, 1994;Carobene, 2003;Cucci, 2004;Dumas and Raffy, 2004;Zecchin et al, 2004b;Nalin et al, 2007;Zecchin et al, 2009Zecchin et al, , 2010aZecchin et al, ,b, 2011b.…”
Section: The Impact Of Glacio-eustasymentioning
confidence: 99%
“…They are linked to glacio‐eustatic changes (Zecchin et al. , 2004; Nalin et al. , 2007), which are correlatable with the deep‐marine stratigraphy based on the δ 18 O record tuned to the Milankovitch orbital parameters (e.g.…”
Section: Introductionmentioning
confidence: 99%