( good ) This new geotectonic function off Greece (changed of Reilinger mais aussi al. [ 58 ], and you may Vott mais aussi al. [ 67 ]) portraying the location of the analysis area and ( b ) mountain shady map of one’s data urban area produced from topographic maps during the step 1:5000 scale of one’s Hellenic Military Geographical Solution.
Geological map of studies urban area modified from Theodoropoulos [ 51 ], IGME [ 68 ], and you can Lekkas et al. [ 69 ]. Fault kinematics try undifferentiated, and most flaws is actually lifeless.
Schematic expression of your uncertainties considered to the enough time-title uplift rates estimations, and the newest correlation of the aquatic terraces having prior sea-height highstands. Elizabeth is the expose-go out height of interior side of the latest terrace, Good ‘s the ages of the brand new patio, age represents this new elevation of your sea-level on duration of terrace development, and delta icons (?) depict the newest projected suspicion on additional parameters. The newest ple.
Coloured arrows (same shade while the Shape cuatro ) suggest terraces T1, T2, T3, T4, T5, T6, T8, and you will T9 ( b ) Look at the newest paleo-coastline perspective out of patio T3 (comparable to MIS 5e ocean-height highstand) northern of Cape Punta
Geographical distribution of your uplifted marine terraces of wide Neapolis town, southeastern Peloponnese. The region of the topographic profiles, while the location of the OSL samples, are illustrated.
( an effective ) Look at the new trip out-of aquatic terraces northwest of Cape Punta. ( c ) Character look at the fresh new patio series into the west section of the fresh new Elafonissos Island ( d ) View of the inner edge of terrace T3 (equal to MIS 5a ocean-top highstand) at the north part of Elafonissos. ( elizabeth ) Outcrop away from Patio T5 caprock, northwest from Cape Punta. View of the inner edge of patio T3 (equal to MIS 5e ocean-top highstand) northeast away from Profitis Ilias.
Three topographic profiles constructed dos.step three kilometer northwest from Cape Punta (Profile A beneficial), within western area of the Elafonissos Area (Character B), and you can cuatro.six kilometer south of Neapolis (Reputation C). To own cities of your pages, come across map in the Shape 4 . This new marine terraces is actually designated repeatedly, beginning with a reduced that. The latest elevations of your interior sides to your terraces, as produced from the fresh new topographic users, are given. The spot and also the age this new OSL products, as well as the MIS related to for every marine terrace, also are provided.
Correlation diagram of these two OSL dated samples, gathered from aquatic terraces T3 and you may T5, correspondingly, that have later Quaternary MIS. Gray vertical groups correspond to the age the quantity of the some other sea-level highstands (of Lisiecki and you will Raymo [ 88 ]). Mean, limit, and you can minimal uplift prices using this relationship also are shown.
The positioning of one’s sedimentary block sample N accumulated to own OSL relationship is even represented ( f )
( a great , b ) Uplifted scrape platforms ranging from Profitis Ilias and Agia Marina, supported by the lowest, steep cliff that have good tidal notch on their legs. ( c babel profili, d ) Uplifted scrape programs at the Agia Marina.
Comparative drawing of your forecast/expected aquatic terraces’ interior edge elevations’ range (designated by the thick black contours) and the noticed internal edge height ranges (marked because of the narrow red-colored traces) with the larger Neapolis urban area. This new predicted level range of one’s internal edges (palaeo-shorelines) for every single MIS were determined underneath the assumption that the enough time-name uplift rate (0.thirty-six ± 0.eleven mm a good ?1 ) is actually constant going back 401 ± ten ka and you will looking at this increase of each MIS highstand (centered on Lisiecki and you may Raymo [ 88 ]-marked here because the gray straight rings), and restriction and minimal condition out-of eustatic sea-height for every MIS highstand (predicated on water-height curve by the Waelbroeck mais aussi al. [ 25 ]).