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Register a new userDetermination of the /M/ reflector which marks the top Messinian at Lattakia region (Land and sea) from seismic profiles
تحديد استمرارية العاكس/M /المسينيان على اليابسة و في البحر في رقعة اللاذقية من البروفيلات السيزمية المتوفرة
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Tishreen University ورقة بحثية
Publication date
2014
fields
Geology
and research's language is
العربية
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Shamra Editor
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أجريت دراسة جيولوجية جيوفيزيائية على أمكنة انتشار جص المسينيان (العاكس السيزمي) على أعماق متباينة في منطقة البحث على اليابسة – شرق اللاذقية أو تحت قاع البحر الأبيض المتوسط – غرب اللاذقية و أدى النشاط التكتوني خلال المسينيان إلى تحول البحر المتوسط إلى حوض ملحي و قد تأثرت منطقة شمال غرب سورية بأزمة المسينيان نتيجة تراجع مياه البحر عنها و تشكل لاغونات تم رفع عدد من البروفيلات الجيولوجية مماسمح تتبع السطح العاكس الممثل بالمتبخرات و تحديد أمكنة انتشار الجص من خلال ربط المقاطع الجيولوجية على اليابسة بالبروفيلات السيزمية البحرية و مضاهاتها مع الآبار المحفورة في رقعة اللاذقية مع الوحدات السيزمية المحددة من قبل (Hall et al., 2005).
A geological geophysical study was carried out to determine positions of gypsum Messinian (seismic reflector) at different depths on land (eastern Lattakia) and under the seabed of western Lattakia During Messinian the tectonic action changed Mediterranean Sea to evaporated basin. Northwestern Syria was affected by salinity crisis because sea water regret from it and due to that it formed lagoons. The establishment of geological sections allowed to determine reflector surface and gypsum positions by linking geological sections on land to marine seismic profiles and correlating it with drilled wells in Lattakia and seismic unites determined by (Hall et al., 2005).
References used
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(BLANKENHORN, M. Gründzüge der geologie und physikalischen geographie von Nordsyrien, Berlin (1891
AL ABDALLA., Présentée à l’université Pierre et Marie Curie En vue de l’obtention du diplôme de.,2008
J BENKHELILl a,∗ M BAYERLY b S BRANCHOUX a, T COURP a, E GONTHIER c, C HUBSCHER d, A Maillard e, E TAHCHI a. la branche orientale de I arc de chypre .Morphostructure d ,une frontiere de plaques d apres les resultats de la la campugne Black (2003). Comptes Rendus Geosciences.2005 ,337,12, 1075-1083
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