Difference between revisions of "Subregional and local pressure compartments"
Jump to navigation
Jump to search
Cwhitehurst (talk | contribs) |
FWhitehurst (talk | contribs) |
||
| Line 14: | Line 14: | ||
| isbn = 0-89181-602-X | | isbn = 0-89181-602-X | ||
}} | }} | ||
| − | Subregional or local (second- and third-order) pressure compartments can be found within normal pressure regimes or regional pressure compartments. | + | Subregional or local (second- and third-order) [[pressure compartments]] can be found within normal pressure regimes or [[regional pressure compartments]]. |
==Subregional pressure compartments== | ==Subregional pressure compartments== | ||
| Line 20: | Line 20: | ||
[[file:formation-fluid-pressure-and-its-application_fig5-26.png|thumb|{{figure number|1}}.]] | [[file:formation-fluid-pressure-and-its-application_fig5-26.png|thumb|{{figure number|1}}.]] | ||
| − | [[:file:formation-fluid-pressure-and-its-application_fig5-26.png|Figure 1]] is an example of a subregional compartment contained within the regional pressure compartment of the Anadarko basin of Figure 5-25. | + | [[:file:formation-fluid-pressure-and-its-application_fig5-26.png|Figure 1]] is an example of a subregional compartment contained within the regional pressure compartment of the [[Anadarko basin]] of Figure 5-25. |
==Local pressure compartments== | ==Local pressure compartments== | ||
| Line 26: | Line 26: | ||
[[file:formation-fluid-pressure-and-its-application_fig5-27.png|thumb|{{figure number|2}}See text for explanation.]] | [[file:formation-fluid-pressure-and-its-application_fig5-27.png|thumb|{{figure number|2}}See text for explanation.]] | ||
| − | The fluids in a porous bioherm completely encased in shale (as shown in [[:file:formation-fluid-pressure-and-its-application_fig5-27.png|Figure 2]]) are virtually isolated from the nearby fluid systems outside the bioherm. The bioherm, then, is a pressure compartment that may or may not be abnormally pressured. Other geological features that may form local pressure compartments are fault blocks, sand lenses, and sand wedges developed in growth | + | The fluids in a [[Porosity#Carbonate pore systems|porous]] [[bioherm]] completely encased in shale (as shown in [[:file:formation-fluid-pressure-and-its-application_fig5-27.png|Figure 2]]) are virtually isolated from the nearby fluid systems outside the bioherm. The bioherm, then, is a pressure compartment that may or may not be abnormally pressured. Other geological features that may form local pressure compartments are fault blocks, sand lenses, and sand wedges developed in [[growth fault]]s. |
==See also== | ==See also== | ||
Revision as of 21:01, 8 May 2014
| Exploring for Oil and Gas Traps | |
| |
| Series | Treatise in Petroleum Geology |
|---|---|
| Part | Critical elements of the petroleum system |
| Chapter | Formation fluid pressure and its application |
| Author | Edward A. Beaumont, Forrest Fiedler |
| Link | Web page |
| Store | AAPG Store |
Subregional or local (second- and third-order) pressure compartments can be found within normal pressure regimes or regional pressure compartments.
Subregional pressure compartments
Figure 1 is an example of a subregional compartment contained within the regional pressure compartment of the Anadarko basin of Figure 5-25.
Local pressure compartments
The fluids in a porous bioherm completely encased in shale (as shown in Figure 2) are virtually isolated from the nearby fluid systems outside the bioherm. The bioherm, then, is a pressure compartment that may or may not be abnormally pressured. Other geological features that may form local pressure compartments are fault blocks, sand lenses, and sand wedges developed in growth faults.
See also
- Pressure compartments
- Regional pressure compartments
- Pressure compartment seals
- Applying pressure compartment concepts to exploration
External links
| find literature about Subregional and local pressure compartments |
|
|
|
|