1976
DOI: 10.1127/zdgg/127/1976/447
|View full text |Cite
|
Sign up to set email alerts
|

A Synoptic View on the Neotectonic Development of the Peloponnesian Coastal Regions

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
16
0
8

Year Published

1990
1990
2013
2013

Publication Types

Select...
5
3
1

Relationship

0
9

Authors

Journals

citations
Cited by 47 publications
(24 citation statements)
references
References 0 publications
0
16
0
8
Order By: Relevance
“…The fossil fauna of this marine Pleistocene is very distinctive in appearance. Corals and thickshelled oysters are common and the shells of gastropods, cockles (Cerastoderma), and other bivalves are much bigger and thicker than the Holocene fossil and living fauna, as has been commonly noted for Tyrrhenian and earlier faunas in the Mediterranean (e.g., Butzer, 1975;Kelletat and Gassert, 1975;Kelletat et al, 1976;Keraudren, 1970Keraudren, , 1971). The middle Holocene and at least five transgressive marine units can be identified in the deep Greek borings (Fig.…”
Section: Coastal Plain Stratigraphymentioning
confidence: 94%
See 1 more Smart Citation
“…The fossil fauna of this marine Pleistocene is very distinctive in appearance. Corals and thickshelled oysters are common and the shells of gastropods, cockles (Cerastoderma), and other bivalves are much bigger and thicker than the Holocene fossil and living fauna, as has been commonly noted for Tyrrhenian and earlier faunas in the Mediterranean (e.g., Butzer, 1975;Kelletat and Gassert, 1975;Kelletat et al, 1976;Keraudren, 1970Keraudren, , 1971). The middle Holocene and at least five transgressive marine units can be identified in the deep Greek borings (Fig.…”
Section: Coastal Plain Stratigraphymentioning
confidence: 94%
“…However, the deep borings in the Argive Plain penetrated more than several hundred meters of Pleistocene deposits indicating considerable subsidence. Raised Tyrrhenian beaches (Kelletat et al, 1976;Schroder and Kelletat, 1976) imply Late Quaternary uplift of the margins of the trough (and/or subsidence of its center). Flemming (1978;Flemming and Webb, 1986), on the other hand, used coastal archaeological sites to place the Argive Plain and nearshore zone inside the 0 m/1000 yr subsidence contour.…”
Section: Topography and Geology Of The Regionmentioning
confidence: 99%
“…Από γεωδαιτικά στοιχεία και τις µεταβολές της στάθµης της θάλασσας που διαπιστώνονται από αρχαιολογικά ευρήµατα, η περιοχή της Βόρειας Πελοποννήσου παρουσιάζει µία γενική ανύψωση καθ' όλη τη διάρκεια του Τεταρτογενούς, που συνεχίζεται και σήµερα (Dufaure, et al, 1979;Kelletat et al, 1978;Mariolakos et al, 1985;Μαριολάκος & Στείρος, 1989). Η ανύψωση αυτή δεν είναι οµοιόµορφη αλλά αντικλινικού τύπου και αυξάνει από Α προς ∆.…”
Section: τεκτονικήunclassified
“…Από αυτή την εποχή και εντεύθεν δημοσιεύθηκε ένα πλήθος μελετών από Ελληνες και ξένους γεωεπιστήμονες με έμφαση σε θέματα Γεωμορφολογίας, Παλαιογεωγραφίας, Γεωλογίας του Τεταρτογενούς, Στρωματογραφίας, Νεοτεκτονικής και Σεισμικότητας, αναφερόμενες στη Δυτ. Μάνη : Hagedorn, (1970), Keraudren, (1970), Kelletat, (1974, Kelletat & Gassert, (1975a, 1975b, Kelletat et al, (1976), Βεργίνης κ. ά., (1975), Stoc ker, (1976, Kowalczyk et al, (1976), Dufaure, (1977), Thiebault, (1977a, 1977b, Angelier & Le Pichon, (1978), Kowalc zyk & Winter, (1979), Riedl, (1979), Φυτρολάκης, (1980, Lyberis & Lalletnant, (1985), Mariolakos et al, (1985) κ.ά.…”
Section: προσδιορισμοί ορυκτών με περιθλασιμετρία (Xrd)unclassified