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Volume 24 Issue 3
Jun 2013
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Article Contents
Constantin Athanassas, Ioannis FOUNTOULIS. Quaternary Neotectonic Configuration of the Southwestern Peloponnese, Greece, Based on Luminescence Ages of Marine Terraces. Journal of Earth Science, 2013, 24(3): 410-427. doi: 10.1007/s12583-013-0334-1
Citation: Constantin Athanassas, Ioannis FOUNTOULIS. Quaternary Neotectonic Configuration of the Southwestern Peloponnese, Greece, Based on Luminescence Ages of Marine Terraces. Journal of Earth Science, 2013, 24(3): 410-427. doi: 10.1007/s12583-013-0334-1

Quaternary Neotectonic Configuration of the Southwestern Peloponnese, Greece, Based on Luminescence Ages of Marine Terraces

doi: 10.1007/s12583-013-0334-1
Funds:

the State Scholarships Foundation of Greece 1500521537.008.040

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  • Corresponding author: Constantin Athanassas, athanassas@ims.demokritos.gr
  • Received Date: 09 Apr 2012
  • Accepted Date: 11 Jun 2012
  • Publish Date: 01 Jun 2013
  • This project studies marine terraces in western Messenia, southwestern Peloponnese, Greece, to propose a model of neotectonic configuration and paleogeographic evolution of western Messenia during the Quaternary. GIS analysis of topographic data and geological mapping revealed flanks of raised terraces created on Quaternary marine deposits. Luminescence ages of sediments from the three westernmost marine terraces tend to be consistent OIS-5, OIS-7 and OIS-9, respectively, thus agreeing with the three latest warm stages of the Pleistocene. Moreover, the type and the extent of deformation of the dated marine terraces allowed us to reflect on the neotectonic configuration of western Messenia as well as to conclude that progressive differential uplift over the last 300 ka has induced a dome-like structure to the upper crust of western Messenia.

     

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