Quaternary Neotectonic Configuration of the Southwestern Peloponnese, Greece, Based on Luminescence Ages of Marine Terraces
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 terra...
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| Veröffentlicht in: | Journal of earth science (Wuhan, China) China), 2013-06, Vol.24 (3), p.410-427 |
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| container_title | Journal of earth science (Wuhan, China) |
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| creator | Athanassas, Constantin Fountoulis, Ioannis |
| description | 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. |
| doi_str_mv | 10.1007/s12583-013-0334-1 |
| format | Article |
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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. 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Earth Sci</addtitle><addtitle>JOURNAL OF EARTH SCIENCE</addtitle><description>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. 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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.</abstract><cop>China University of Geosciences</cop><pub>China University of Geosciences</pub><doi>10.1007/s12583-013-0334-1</doi><tpages>18</tpages></addata></record> |
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| ispartof | Journal of earth science (Wuhan, China), 2013-06, Vol.24 (3), p.410-427 |
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| subjects | Biogeosciences Earth and Environmental Science Earth science Earth Sciences Geochemistry Geologic mapping Geology Geotechnical Engineering & Applied Earth Sciences Luminescence Marine biology Plate tectonics Pleistocene Quaternary Terraces 光时 古地理演化 希腊 新构造 海岸 第四纪 西南部 配置 |
| title | Quaternary Neotectonic Configuration of the Southwestern Peloponnese, Greece, Based on Luminescence Ages of Marine Terraces |
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