( an effective ) Brand new geotectonic form from Greece (changed of Reilinger mais aussi al. [ 58 ], and Vott ainsi que al. [ 67 ]) portraying the location of investigation town and you can ( b ) hill shady map of your own investigation area made out of topographic maps on 1:5000 level of your Hellenic Armed forces Geographical Solution.
Geological chart of studies area modified away from Theodoropoulos [ 51 ], IGME [ 68 ], and you will Lekkas ainsi que al. [ 69 ]. Blame kinematics are undifferentiated, and more than faults try deceased.
Schematic icon of your concerns considered toward a lot of time-term uplift prices estimations, and also for the new relationship of your aquatic terraces having previous water-peak highstands. E ‘s the expose-time height of one’s inner side of the terrace, A 
beneficial ‘s the age of new patio, elizabeth corresponds to the fresh level of one’s sea level within duration of terrace creation, and the delta icons (?) portray this new projected uncertainty regarding the various other parameters. The fresh new ple.
Colored arrows (exact same tone once the Contour cuatro ) indicate terraces T1, T2, T3, T4, T5, T6, T8, and T9 ( b ) View of the fresh paleo-coastline direction from patio T3 (comparable to MIS 5e sea-peak highstand) northern of Cape Punta
Geographic shipping of uplifted marine terraces of your broader Neapolis area, southeastern Peloponnese. The location of topographic users, as well as the located area of the OSL products, are portrayed.
( an effective ) Look at the fresh new trip out of marine terraces northwest out-of Cape Punta. ( c ) Profile view of the newest terrace succession into the western part of this new Elafonissos Island ( d ) View of the internal edge of patio T3 (corresponding to MIS 5a ocean-level highstand) during the northern section of Elafonissos. ( e ) Outcrop away from Terrace T5 caprock, northwest regarding Cape Punta. Look at the internal side of patio T3 (corresponding to MIS 5e ocean-level highstand) northeast away from Profitis Ilias.
About three topographic profiles created 2.step 3 kilometer northwest from Cape Punta (Reputation An excellent), on western part of the Elafonissos Isle (Character B), and you may cuatro.six kilometres southern out-of Neapolis (Profile C). To own places of the users, see map within the Figure 4 . The newest marine terraces is designated repeatedly, starting with a decreased you to definitely. The new elevations of one’s internal corners to your terraces, because produced from new topographic profiles, are provided. The location therefore the chronilogical age of the new OSL products, and the MIS caused by per aquatic patio, also are offered.
Correlation diagram of these two OSL old products, gathered out-of aquatic terraces T3 and you will T5, respectively, with later Quaternary MIS. Gray vertical rings match the age the amount of various other sea-height highstands (out-of Lisiecki and you may Raymo [ 88 ]). Indicate, limitation, and you can lowest uplift prices out of this correlation are also revealed.
The position of one’s sedimentary cut-off attempt N obtained having OSL dating is additionally represented ( f )
( good , b ) Uplifted scratch networks ranging from Profitis Ilias and you will Agia Marina, backed by a minimal, high cliff which have an excellent tidal notch during the their base. ( c , d ) Uplifted abrasion networks during the Agia Marina.
Comparative diagram of predict/asked aquatic terraces’ internal boundary elevations’ ranges (designated from the heavy black colored outlines) therefore the observed inner edge height selections (designated by slim purple outlines) towards the wide Neapolis town. This new predicted height range of the internal corners (palaeo-shorelines) each MIS was indeed calculated beneath the assumption your much time-name uplift speed (0.36 ± 0.eleven mm good ?1 ) try ongoing for the last 401 ± ten ka and you can taking into consideration this increase of any MIS highstand (based on Lisiecki and Raymo [ 88 ]-marked right here due to the fact gray straight groups), in addition to maximum and you may minimum standing out-of eustatic sea-level for every MIS highstand (based on sea-top contour of the Waelbroeck et al. [ twenty five ]).
