Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Analysis of Overpressure Mechanisms in a Field of Southwestern Malay Basin

View through CrossRef
This study demonstrate the utilization of wireline logs for pore pressure mechanism analysis in a field of southeastern Malay basin. Development of overpressures means that fluid movement in the pores is retarded both vertically and laterally. Detailed knowledge of lithology, rock history, and pressure mechanism is important for overpressure prediction. In many tertiary basins overpressure is mainly generated by compaction disequilibrium due to high deposition rate and low permeability in shales. In Malay basin, temperature also plays an important role in generating overpressure at shallow depth as geothermal gradient is very high 40-60 oC. Pore pressure data from 10 wells is used to for mechanism analysis. Overburden pressure is calculated for all the wells by using density log and sonic velocity-vertical effective stress, vertical effective stress-density and pore pressure cross plots are used for mechanism analysis. The results obtained from the cross plots reveal that in the study area overpressure is generated by both primary (undercompaction) and secondary mechanism such as chemical compaction and fluid expansion/hydrocarbon generation in different wells. Overpressure magnitude analysis suggests that overpressure generated due to secondary mechanism is very high as compare to primary mechanism. Eaton's method with exponent 3 for sonic velocity under-predicted the pore pressure in the wells where both primary and secondary mechanism are present but in such wells pore pressures are reasonably predicted by using higher Eaton exponent. Overpressure behavior is very complex in the study area, in some wells it start at shallow depth and increase gradually with depth whereas in some wells it start at greater depth and ramp up quickly, this complex behavior also shows the presence of different mechanisms. For the safe drilling and completing the well economically, knowledge of overpressure is essential. Overpressure mechanism analysis is very important for overpressure prediction and it will help in understanding the behavior of pore pressure and applying the appropriate prediction method .?Accurate overpressure prediction is very important for construction of deep water seafloor facilities in HPHT environments.
Title: Analysis of Overpressure Mechanisms in a Field of Southwestern Malay Basin
Description:
This study demonstrate the utilization of wireline logs for pore pressure mechanism analysis in a field of southeastern Malay basin.
Development of overpressures means that fluid movement in the pores is retarded both vertically and laterally.
Detailed knowledge of lithology, rock history, and pressure mechanism is important for overpressure prediction.
In many tertiary basins overpressure is mainly generated by compaction disequilibrium due to high deposition rate and low permeability in shales.
In Malay basin, temperature also plays an important role in generating overpressure at shallow depth as geothermal gradient is very high 40-60 oC.
Pore pressure data from 10 wells is used to for mechanism analysis.
Overburden pressure is calculated for all the wells by using density log and sonic velocity-vertical effective stress, vertical effective stress-density and pore pressure cross plots are used for mechanism analysis.
The results obtained from the cross plots reveal that in the study area overpressure is generated by both primary (undercompaction) and secondary mechanism such as chemical compaction and fluid expansion/hydrocarbon generation in different wells.
Overpressure magnitude analysis suggests that overpressure generated due to secondary mechanism is very high as compare to primary mechanism.
Eaton's method with exponent 3 for sonic velocity under-predicted the pore pressure in the wells where both primary and secondary mechanism are present but in such wells pore pressures are reasonably predicted by using higher Eaton exponent.
Overpressure behavior is very complex in the study area, in some wells it start at shallow depth and increase gradually with depth whereas in some wells it start at greater depth and ramp up quickly, this complex behavior also shows the presence of different mechanisms.
For the safe drilling and completing the well economically, knowledge of overpressure is essential.
Overpressure mechanism analysis is very important for overpressure prediction and it will help in understanding the behavior of pore pressure and applying the appropriate prediction method .
?Accurate overpressure prediction is very important for construction of deep water seafloor facilities in HPHT environments.

Related Results

Cosmopolitan Musical Expressions Of Malay Indigeneity In Singapore
Cosmopolitan Musical Expressions Of Malay Indigeneity In Singapore
<p><strong>Over the past ten years, the activities of Malay composers with backgrounds in traditional music has been steadily increasing within the Malay traditional mu...
Modeling of Overpressure Generation–Evolution of the Paleogene Source Rock and Implications for the Linnan Sag, Eastern China
Modeling of Overpressure Generation–Evolution of the Paleogene Source Rock and Implications for the Linnan Sag, Eastern China
Subsurface pore pressure affects the direction of hydrocarbon migration, determines the distribution of the hydrocarbon reservoir, and provides scientific reference for drilling pl...
Characteristics of Overpressure Systems and Their Significance in Hydrocarbon Accumulation in the Yinggehai and Qiongdongnan Basins, China
Characteristics of Overpressure Systems and Their Significance in Hydrocarbon Accumulation in the Yinggehai and Qiongdongnan Basins, China
Abstract Overpressure systems are widely developed in the central depression and palco‐uplift in the Yinggehai and Qiongdongnan basins. They can be divided into three types accordi...
Thomas Bowrey (1701) 17th Century Description of Malay
Thomas Bowrey (1701) 17th Century Description of Malay
Thomas Bowrey, who was an employee of the British colonial government, visited the Malay-speaking region at the end of the 17th century and published a dictionary of Malay (1701) w...
Origin of Overpressure and Its Influence on Hydrocarbon Leakage in Mosuowan Uplift of the Junggar Basin, NW China
Origin of Overpressure and Its Influence on Hydrocarbon Leakage in Mosuowan Uplift of the Junggar Basin, NW China
ABSTRACT The Junggar Basin is one of the main petroliferous basins in Western China. The Mosuowan Uplift, located in the central part of the Junggar Basin, is a f...
DETECTING OVERPRESSURE ZONES USING MODEL-BASED SEISMIC INVERSION: A CASE STUDY FROM SRIKAIL-01 WELL, SRIKAIL GAS FIELD, BANGLADESH
DETECTING OVERPRESSURE ZONES USING MODEL-BASED SEISMIC INVERSION: A CASE STUDY FROM SRIKAIL-01 WELL, SRIKAIL GAS FIELD, BANGLADESH
An overpressure zone is critical in petroleum exploration drilling, leading to potentially dangerous blowouts and other drilling-related hazards. Yet, it often contains significant...
The Origin of Overpressure in the Pinghu Tectonic Zone of Xihu Depression and Its Relationship with Hydrocarbon Accumulation
The Origin of Overpressure in the Pinghu Tectonic Zone of Xihu Depression and Its Relationship with Hydrocarbon Accumulation
Clarification of the cause of overpressure is of great significance for the study of hydrocarbon generation, migration and accumulation processes under an overpressure environment,...
High-temperature overpressure basin reservoir and pressure prediction model
High-temperature overpressure basin reservoir and pressure prediction model
Yinggehai Basin locates in the northern South China Sea. Since the Cainozoic Era, crust has several strong tension, the basin subsides quickly, the deposition is thick, the crust i...

Back to Top