Do you want to publish a course? Click here

A sedimentary conditions and reservoir characterization study of Juriba & transition zone formation in ELmhash structure using micro slides and geophysical well Logging

دراسة الوضع الترسيبي و الصفات الخزنية لتشكيلتي الجريبة و الانتقالية في تركيب المهاش باستخدام الشرائح المجهرية و القياسات الجيوفيزيائية البئرية

911   1   156   0 ( 0 )
 Publication date 2016
and research's language is العربية
 Created by Shamra Editor




Ask ChatGPT about the research

This research highlights on new manner in study of petroleum reservoir , by integrated between a sedimentary study, which comprises micro slides from side, and geophysical well logging interpretation from another side, in Juriba & Transition zone formation, in ELmhash structure oil field , at Euphrates depression – west DER Azzor -Syria. A selection (5) wells in ELmhash structure is Mahash (17-18-11-4- 7).

References used
BATHURST,C1975-Carbonate sediment and their diagenesis. 2nd, Amsterdam, 658 p
CHILINGER,G1967,BISSEL,H1967,andWOLD,K,1967-The diagenesis of carbonate rocks.Elsevier Publ, Amsterdam, 471p
DUNHAM, R1962- Classification of Carbonate rock according to depositional texture in Ham, W. E. (ed) classification of carbonate rocks, Am. Asso. Pet. Geol. Mem. 1, pp: 108-121
rate research

Read More

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.
many potentially prolific producers have already been plugged and abandoned , owing to lack of adequate formation evaluation . For example , In the early days of log analysis، it was common practice to regard water saturations above 50% as non-com mercial. However, with advances in logging and seismic technology came the realization that some of those supposedly non-commercial zones were، in fact، highly productive pays , depending on pore-size distributionof the rock , movable or immovable fluids and production probability .
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.
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.
In this research we have synthesized a new macrocyclic Schiff base (II) containing nitrogen- oxygen donor atoms which was designed and synthesized by reaction of: 1,4– bis (6',6'- methoxy -3- formyl phenyl)-1,4- dioxa butane (I). Identification of this macrocyclic schiff base: (II) 1,16- Diaza–[3,6;11,14-di (6',6'- methoxy phenyl)]-7,10,19,22 - tetraoxa cyclo tetra icozane-15,1dien was determined by (LC-MS) and spectroscopy (IR). The liquid- liquid extraction of metal such as Zn2+, Pb2+ and Ni2+ from aqueous phase to organic phase which doesn't in water. The effect of chloroform and dichloromethane as organic solvents over the metal extractions was investigated at 25± 0.10C by using atomic absorption Spectrometer and extraction percentage was calculated.
comments
Fetching comments Fetching comments
mircosoft-partner

هل ترغب بارسال اشعارات عن اخر التحديثات في شمرا-اكاديميا