2016
DOI: 10.1111/ter.12203
|View full text |Cite
|
Sign up to set email alerts
|

Fluid overpressure as a control on sandstone reservoir quality in a mechanical compaction dominated setting: Magnolia Field, Gulf of Mexico

Abstract: The reservoir quality (porosity and permeability) of deeply buried hydrocarbon reservoir sandstones in sedimentary basins is significantly affected by burial diagenesis. Many deep reservoirs develop anomalous fluid overpressures during burial. Previous studies on the effect of fluid overpressure on reservoir quality in these deep reservoirs have been inconclusive because of the difficulty in constraining the individual contributions of various porosity preserving factors that are simultaneously active in these… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

1
19
0

Year Published

2016
2016
2024
2024

Publication Types

Select...
7

Relationship

2
5

Authors

Journals

citations
Cited by 20 publications
(20 citation statements)
references
References 34 publications
(47 reference statements)
1
19
0
Order By: Relevance
“…This in part is due to the significant role low VES plays in limiting and forestalling the onset of intergranular pressure solution at grain contacts (e.g. Osborne and Swarbrick, 1999;Swarbrick et al, 2000;Sheldon et al, 2003;Becker et al, 2010 Stricker andJones 2016). Quartz cementation and especially quartz overgrowths on detrital quartz grains are a widely reported diagenetic and porosity reducing processes in deeply buried quartz rich sandstones (e.g.…”
Section: A C C E P T E D Accepted Manuscriptmentioning
confidence: 99%
“…This in part is due to the significant role low VES plays in limiting and forestalling the onset of intergranular pressure solution at grain contacts (e.g. Osborne and Swarbrick, 1999;Swarbrick et al, 2000;Sheldon et al, 2003;Becker et al, 2010 Stricker andJones 2016). Quartz cementation and especially quartz overgrowths on detrital quartz grains are a widely reported diagenetic and porosity reducing processes in deeply buried quartz rich sandstones (e.g.…”
Section: A C C E P T E D Accepted Manuscriptmentioning
confidence: 99%
“…After fluid overpressure is formed, thick mudstone can adequately seal sandstone pore fluids and form a series of vertical pressure compartments with 18 Geofluids independent fluid pressures accompanied with compaction and clay mineral conversion at a late stage of diagenesis. These compartments are not connected with the upper hydrodynamic system [45]. The pore fluids in closed overpressure systems support part of the load of the overlying strata and reduce the vertical effective stress and the pressure supported by framework particles and cements.…”
Section: Early-stage Overpressure With the Formation Of Chlorite Coatmentioning
confidence: 99%
“…Hudec and Jackson 2007;Archer et al 2012;Hudec et al 2013;Sathar and Jones 2016). Such studies have increased our understanding of salt movement, the development of salt-walled mini-basins and on the effects of coeval halokinesis on sedimentary Edited by Jie Hao processes and facies distribution (e.g.…”
Section: Introductionmentioning
confidence: 99%