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Tectono- Seismic study of Kurachine dolomite in Sadad structure- Al- Daw depression

دراسة تكتونو – سيزمية لتشكيلة الكوراشينا دولوميت في تركيب صدد – حوض الدو

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 Publication date 2018
  fields Geology
and research's language is العربية
 Created by Shamra Editor




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In this paper, we will shed light on the applied studies results in special of deep tectonic situation of the Kurachine dolomite formation through the seismic sections explained by us, and establish time and depth maps for this formation, and proposing a well that is supposed to be hydrocarbon potential in the light of modern data.

References used
Al Abdalla,A.(2008) – Tictonic evalution of Arabian plate in Syria since Mesozoic , PhD thesis. Paris, France. 302p
Cavazza, W., Roure, F., Spakman, Stampfli, G.M. and Ziegler, P.A., eds. (2004a) - The TRANSMED Atlas: The Mediterranean Region form Crust to Mantle: Heidelberg, Springer-Verlag, 141 pp. + CD-ROM
Beydoun,Z.R. (1991) – Arabian plate hydrocarbon geology and potential , a plate tectonic approach. American Association of geology, studies in geology. Geologist Bulletin, v77, pp 173-193
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Abo Rabah is one of the most important structures in the Al- Daw basin, because of the great tectonic complexity that has been exposed during the geological history, and being one of the most important gas producing areas in Syria. That explains t he importance of its study. Our applied studies indicates that there is significant variation in salt thickness depending on sedimentation and tectonic factors, which directly affects the kurachine dolomite gas reservoir, Here lies the importance of this paper.
This research aims to study the sedimentary and palaeogeographic evolution of the Kurachina Dolomite Formation along Palmyrian belt zone. Studying this formation in its Northern and Southern parts has shown that it consists of two lithostratigraph ic members, where each of them includes a series of lithological units. The petrological study of the components of these units shows that they are composed of four distinguished facies: Dolomitic limestones, clayey limestones, clays and anhydrites, pure or mixed, and deposited in repeated harmonic layers, gathered mostly in neutral sedimentary sequences. Dolomitic limestones are the most common and important facies, they are composed of micrite muds which have been subjected, in different degrees to synsedimentary or late dolomitisation processes through pumping or burial mechanisms. Dolomitisation intensity decreases downward the formation and increases laterally from the south to the north of the Palmyrian chain.
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All the well logging reinterpretation by using the new softwares, cores analysis and results of seismic 2D and 3D surveys allowed to identify the reservoir characteristics of Kurachina Dolomite Formation of middle Triassic, for two zones (C2, D1) in Jihar field and its affect on hydrocarbon potential in this area. It's found that C2 reservoir consist mostly of dolomite and small amount of shale and anhydrite, fractured and all the fractures are full of organic materials, calcite, anhydrite, silica and little amount of stilolite, while there is succession of limestone and fossil remains, in some places there is shally dolomite. Whereas D1 reservoir is mostly crystalline limestone and the fractures filled with dolomite.
The available seismic data of Mamlaht Al-Kom field were reinterpreted in order to define some petroleum potential reflections. The study focused on Korushina Dolomite (K.D) reflector because of its properties that indicate α hydrocarbon potential. Therefore the time map of this formation was canstructed, structure was defined and the hydrocarbon potential is discussed. According to the obtained data, we ensure the presence hydrocarbon potential of the K. D formation, because of its suitable thickness, availability of cover, and the source rocks. These results should be verified by a 3D surveys and then drilling operations.
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