أكدت النتائج، التي تم الحصول عليها من دراسة ١٢٥ عينة من ١٠ آبار مختارة من تشكيلات
الترياسي في شمال شرق سورية، وجود محتبسات مائية و كربونية و هيدروكربونية. سمحت الخصائص
العامة و الفيزيا-كيميائية المتباينة للمحتبسات المائية بتمييز ثلاثة أجيال.
Obtaind results, by studing ١٢٥ samples from ١٠ deep wells covering the
different Triassic formations in NE-Syria,show the existence of various
inclusion types. Aqueous, carbon and hydrocarbon-bearing. Aqueous inclusions
vary widely in their general and physico–chemical features, form, melting and
homogenization temperature, and density of the enclosed fluid.
References used
BILAL . A. (١٩٨٨) –paleothermal study of triassic formations in syria by using fluid inclusions . AAPG Mediterranean , Nice , France
BILAL . A. (١٩٩٢a) –Utilisation of fluid inclusions in petroleum exploration, exemple: Kurachine Dolomite Formation in Al Andalus area, Syria. The eleventh Petroleum Conference , Cairo , Egypt
BILAL. A. (١٩٩٤) –Fluid inclusions application in geology. Exemples from syria . Second inter.cnfe.on geology of the Arab world
The geophysical surveys on the Syrian oil fields had begun since (1933);it
continued by the soviet groups (1952-1962) and were completed by the Syrian
national groups. The Derro oil field had a good lot from these studies, because
it was surveyed
The main objective of this research is to estimate the potential electrical power that can be extracted from closed and out-of-service oil wells situated in the north-eastern part of Syria. The research shows that using Organic Rankine Cycle (ORC) wi
The Palmyra's chain, is one of the Syrian strategic petroleum regions. Thus the
petroleum companies were interested by this structure through the petro-service contracts.
This study focused on petroleum potential of the Mizozoic formations in the N
Geomorphological-chemical studying of hole phenomenon which
taked place in KARKIT village (NE of Lattakia) at 11/2/2009,indicate that it was a result of karstic phenomenons in gypsum rocks,this karst is result of underground water drainage inaccordance with fissures direction In study region N025 .
Shiranish formation in Sazaba Oil fields region had been divided by
Petrology study and well Logs measurements to three major members (lower –
middle – upper). Then these members have been divided to lithostratigraphic
units and subunits. This stu