کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
4696593 | 1351690 | 2006 | 17 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Upper Cenozoic stratigraphy and paleogeographic evolution of Myrtoon and adjacent basins, Aegean Sea, Greece
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
زمین شناسی اقتصادی
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چکیده انگلیسی
The region appears to have progressively subsided since the Miocene. Myrtoon basin and Saronikos Gulf were lake basins in the Messinian that were flooded to form deep-water marine basins during the basal Pliocene transgression. South Evoikos and Argolikos basins were progressively flooded during the Pliocene and early Quaternary. In most areas, deep-marine basins filled principally with hemipelagic sediment, but a submarine fan developed in the early Pliocene in the northern Myrtoon basin and fan deltas built into the basin from the east and southwest. Opening of marine 'gateways' as a result of subsidence led to enhanced oceanographic circulation and the formation of regional erosion surfaces at basin margins.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Marine and Petroleum Geology - Volume 23, Issue 3, April 2006, Pages 353-369
Journal: Marine and Petroleum Geology - Volume 23, Issue 3, April 2006, Pages 353-369
نویسندگان
George Anastasakis, David J.W. Piper, Michael D. Dermitzakis, Vassilios Karakitsios,