The Miocene Gachsaran Formation evaporite cap rock, Zeloi oilfield, SW Iran

2014 ◽  
Vol 30 (3) ◽  
pp. 287-306 ◽  
Author(s):  
Bahman Soleimani ◽  
Alireza Bahadori
Keyword(s):  
Sw Iran ◽  
2021 ◽  
Vol 2 (3) ◽  
pp. 248-257
Author(s):  
Samira Abbasi ◽  
Saeid Pourmorad ◽  
Ashutosh Mohanty

Many problems in the production and development of oil fields lie in the correct and accurate assessment of the reservoir cap rock. Ramshir oil field is located 130 km southeast of Ahvaz and is one of the most important oil fields in the southwest of the country. To evaluate the petrographic and diagenetic properties, 300 thin microscopic sections were studied. According to petrographic studies, it was found that the cap rock in Ramshir oil field is composed of more evaporative sediments (mainly anhydrite with some gypsum) with some non-evaporative sediments (marl, carbonate and bituminous shale). The most important diagenetic processes in the study area were considered to be dolomitization, cementation, compaction, anhydrite, recrystallization and substitution. Petrographic and diagenetic studies suggest a swamp-swamp environment for this environment. Lithological changes are a sign of hot, humid, hot and dry weather during sedimentation of the cap rock of this field. Doi: 10.28991/HEF-2021-02-03-06 Full Text: PDF


2011 ◽  
Vol 148 (5-6) ◽  
pp. 854-867 ◽  
Author(s):  
I. ABDOLLAHIE FARD ◽  
M. SEPEHR ◽  
S. SHERKATI

AbstractWe present and use seismic images to constrain possible scenarios for the evolution of the Middle Miocene Gachsaran Formation in the Central Iranian Zagros during the Neogene folding. This evaporitic sequence plays an important role in sealing the Oligocene–Miocene Asmari reservoirs in the Dezful Embayment and offshore regions. It was deposited in the flexural basin south of the Mountain Front Fault, during the progressive southwestward propagation of the Zagros folding. Its thickness changes very rapidly from several hundred to more than 4000 m. This thickness variation is related to faulting, folding and flow. Seismic and subsurface data show that the Gachsaran evaporite sequence is a major disharmonic level in the Dezful Embayment and shallow, molassic synclines often overlie anticlinal axes at depth. The lithological composition of the Gachsaran Formation is mainly a combination of salt, shale and anhydrite, which have a high interval velocity contrast. Anomalous velocity behaviours of these sedimentary units after deformation affect the seismic quality of the surrounding area, especially the southern flank of the main anticline structures.


2018 ◽  
Vol 11 (1) ◽  
pp. 107-117 ◽  
Author(s):  
Naeimavi Majid ◽  
Khazali Fereydoon ◽  
Abdideh Mohammad ◽  
Zohreh Saadati

Introduction:Gachsaran Formation is the cap rock of Asmari oil reservoir located in southwestern of Iran. The formation consists of halite, anhydrite, and tachyhydrite, The most important feature of this formation is the presence of high-pressure fluid.Method:Drilling companies have to use heavy-weighted mud to drill the high-pressure formation. Sometimes the weight of drilling fluid is used, up to 2.65(gr/cm3). Although heavy-weight mud prevents formation fluid to flow into the well, it is difficult to maintain and control its properties. If the hydrostatic pressure is insufficient, the formation connate fluid penetrates into the drilling mud and contaminates it.Result:The study found that the symptoms of this contamination lead to an increase in calcium, magnesium, carbonates, and bicarbonates levels, as well as a decrease in pH. The drilling fluid rheology also affected by the contamination.Discussion:Then, method of curing this event is discussed. Prevention, the best treatment for this event was introduced. It was also found that, as soon as contamination signs appear, immediately increase the drilling fluid weight as much as possible, and then adjust the pH between 10.5 and 11.5. The maintain method described is continued until section drilling ends.


Author(s):  
Masoud Soleimani ◽  
◽  
Bahman Soleimani ◽  
Bahram Alizadeh ◽  
Iman Veisy ◽  
...  
Keyword(s):  

2011 ◽  
Vol 54 (2) ◽  
pp. 137-147 ◽  
Author(s):  
Mehdi Esfandiari ◽  
MossadeMohammad Saeed Mossadegh ◽  
Parviz Shishehbor
Keyword(s):  

2000 ◽  
Vol 43 (2-4) ◽  
pp. 239-249 ◽  
Author(s):  
S.E Kruse ◽  
J.C Schneider ◽  
D.J Campagna ◽  
J.A Inman ◽  
T.D Hickey

Sign in / Sign up

Export Citation Format

Share Document