کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
6441754 | 1639101 | 2014 | 18 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
The tectono-sedimentary evolution of the Lechaion Gulf, the south eastern branch of the Corinth graben, Greece
ترجمه فارسی عنوان
تحول تکتونو-رسوبی خلیج لشحون، شاخه جنوب شرقی قرنیت گابن، یونان
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کلمات کلیدی
شکاف کریستین، عصاره دانه لخیا خلیج فارس، تکامل رسوبات،
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
ژئوشیمی و پترولوژی
چکیده انگلیسی
The Gulf of Corinth is the second most active continental rift in the world and thus a much-studied natural laboratory for analyzing details of rift history. A new detailed offshore seismic survey combined with previously acquired data in its least studied part, the Lechaion Gulf, shed light on the tectono-sedimentary evolution of the eastern end of the Corinth rift. This study shows that: (i) the Lechaion Gulf is the submerged northern part of the onshore Corinth-Nemea basin, (ii) they are both bounded to the south by the north dipping Klenia and Kenchreai faults, which are considered at present inactive, (iii) both the Corinth-Nemea basin and the Lechaion Gulf were formed at around between 3.6 and 4Â Ma BP (middle to late Pliocene), at the same time with the Megara basin, and (iv) the Lechaion Gulf was submerged and took its present shape at around between 0.7 and 1.7Â Ma BP, at the same time with the Gulf of Corinth and the Alkyonides Gulf. Furthermore, sequence stratigraphy interpretation of seismic profiles from the Lechaion Gulf revealed: (i) a total post-alpine sediment thickness of almost 3Â km below the Lechaion Gulf, (ii) at least 400Â m of sediments accumulated during the last 245Â ka, corresponding to a mean sedimentation rate of 1Â m/ka for the last 245Â ka and 2.3Â m/ka for the Holocene, and (iii) differential vertical movement, in the order of 4.5Â km, between the bedrock under the Lechaion Gulf and the adjacent mountains yields an accumulative average slip rate of 0.9Â m/ka or less, over the last 4Â Ma. Therefore, for estimating more accurately the slip rates, the uplift rates, the extensional rates and the earthquake recurrence interval over the eastern end of the Corinth rift, the presently mentioned tectono-sedimentary evolution of the Lechaion Gulf must be taken into consideration.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Marine Geology - Volume 351, 1 May 2014, Pages 58-75
Journal: Marine Geology - Volume 351, 1 May 2014, Pages 58-75
نویسندگان
Marinos Charalampakis, Vassilis Lykousis, Dimitris Sakellariou, George Papatheodorou, George Ferentinos,