Quaternary evolution of the Corinth Rift and its implications for the Late Cenozoic evolution of the Aegean
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چکیده
منابع مشابه
Tectonosedimentary evolution of the basins in Central Alborz, Iran
Evidence of at least ten different tectonic- controlled sedimentary basins can be recognized in the central part of the Alborz Mountains in the Middle part of the Alpine-Himalayan belt. They formed from Neoprotrozoic to recent time as the results of the relative plate motion in southwest of Asia in Tethyan realm. The basins include: (1) Prototethys Late Neo-Proterozoic to Early Ordovician epi-c...
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