قادت الدراسة التي أُجريت على توضعات النيوجين القارية في كل من منطقتي دمشق و القلمون إلى تمييز تشكيلتين ليتولوجيتين: تشكيلة سفلى مؤلفة من رسوبات حطامية ذات عناصر ناعمة بصورة عامة، يغلب فيها الرمل و الغضار، تنتشر في قاعدتها محلياً بقايا صبة بركانية بازلتية؛ و تشكيلة عليا مؤلفة من رسوبات كونغلوميراتية ذات عناصر خشنة متباينة الحجوم و المصادر.
بينت الدراسة أن الصبات البركانية التي اندفعت من الجنوب، كصبة جبل المانع البازلتي في جنوب دمشق، بلغت الأطراف الجنوبية لحوض الديماس و لم تتعداها بعيداً نحو الشمال.
كما بينت الدراسة أن عمر التوضعات القارية المستقرة فوق الصبات البركانية تعود في قواعدها السفلى إلى عمر الميوسين، و ذلك مقارنة بمعطيات التحاليل النظائرية للصخور البركانية المسجلة سابقاً في المنطقة.
The study of continental Neogene deposits in Damascus and Kalamoun
areas has led to distinguish two lithological formations: the bottom one is
composed of debris with fine elements in general, dominated by sand and clay,
widespread on its base locally remnants of volcanic basalt flow. The top
formation consist of conglomerate sediments with coarse elements of mixed
sizes and sources.
The study showed that volcanic flow which came from the south as basaltic
flow from Al-Manea Mountain to the south of Damascus, reached the southern
part of Dimas Basin and not far beyond it towards the north.
Also, the study demonstrated that the age of the continental deposits
overlying the volcanic flows belong at their bases to Lower Miocene age, in
comparison with the data of the isotopic analysis of the volcanic rocks
previously recorded in the region.
References used
Faradzev V. A. 1966. Geological map of Syria, scale 1 : 200 000, sheet I-37- XIV. Explanatory notes. V. O. Teechnoexport, Moscow
Kurbanov, N. and Zarjanov, Yu., 1966. Geological map of Syria, scale 1: 200 000, sheet I-37-XIV. Explanatory notesTeechnoexport, Moscow
Mouty, M., (in publication). New contribution to the tectonic study of the Palmyrides fold belt, Damascus University Journal
The lithologic and palaeontologic study of the marine Neogene in Salquine
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