Difference between revisions of "Balanced cross sections"

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  | part    = Predicting the occurrence of oil and gas traps
 
  | part    = Predicting the occurrence of oil and gas traps
 
  | chapter = Exploring for structural traps
 
  | chapter = Exploring for structural traps
  | frompg  = 20-1
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  | frompg  = 20-33
  | topg    = 20-70
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  | topg    = 20-34
 
  | author  = R.A. Nelson, T.L. Patton, S. Serra
 
  | author  = R.A. Nelson, T.L. Patton, S. Serra
 
  | link    = http://archives.datapages.com/data/specpubs/beaumont/ch20/ch20.htm
 
  | link    = http://archives.datapages.com/data/specpubs/beaumont/ch20/ch20.htm
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==Definition==
 
==Definition==
  
Balanced cross sections honor all available data and are constructed and analyzed to ensure they are geometrically possible and geologically admissible, given reasonable [[assumptions]] about the predeformation setting of rocks and how rocks behave during [[deformation]] in a particular tectonic environment. “Balanced” refers to the basic assumption made in constructing these sections—that rock area (rock volume) does not change substantially as a result of deformation. Balanced cross sections are restorable. This means that, while maintaining constant area, the deformation displayed in a balanced cross section can be incrementally removed to yield a geologically plausible predeformation configuration.
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Balanced [[cross section]]s honor all available data and are constructed and analyzed to ensure they are geometrically possible and geologically admissible, given reasonable [[assumptions]] about the predeformation setting of rocks and how rocks behave during [[deformation]] in a particular tectonic environment. “Balanced” refers to the basic assumption made in constructing these sections—that rock area (rock volume) does not change substantially as a result of deformation. Balanced cross sections are restorable. This means that, while maintaining constant area, the deformation displayed in a balanced cross section can be incrementally removed to yield a geologically plausible predeformation configuration.
  
 
The constant area (constant volume) assumption is generally valid for deformation that has occurred in upper crustal, nonmetamorphic settings, but there are important exceptions. For example, in some settings syntectonic deposition and compaction can result in substantial rock volume changes throughout the course of deformation. In these cases, approximations of the volume changes must be incorporated in the balancing process.
 
The constant area (constant volume) assumption is generally valid for deformation that has occurred in upper crustal, nonmetamorphic settings, but there are important exceptions. For example, in some settings syntectonic deposition and compaction can result in substantial rock volume changes throughout the course of deformation. In these cases, approximations of the volume changes must be incorporated in the balancing process.
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==Examples of use==
 
==Examples of use==
  
* Buchanan, P. G., Nieuwland, D. A., eds., 1996, Modern Developments in Structural Interpretation, Validation and Modelling: [http://sp.lyellcollection.org/content/99/1 Geological Society of London Special Publication 99], p. 369.
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* Buchanan, P. G., and D. A. Nieuwland, eds., 1996, Modern Developments in Structural Interpretation, Validation and Modelling: [http://sp.lyellcollection.org/content/99/1 Geological Society of London Special Publication 99], p. 369.
 
* Dahlstrom, C. D. A., 1969, Balanced cross sections: Canadian Journal of Earth Sciences, vol. 6, p. 743–757, DOI: [http://www.nrcresearchpress.com/doi/abs/10.1139/e69-069#.Ux4tNOddVQQ 10.1139/e69-069].
 
* Dahlstrom, C. D. A., 1969, Balanced cross sections: Canadian Journal of Earth Sciences, vol. 6, p. 743–757, DOI: [http://www.nrcresearchpress.com/doi/abs/10.1139/e69-069#.Ux4tNOddVQQ 10.1139/e69-069].
* Mount, V. S., Suppe, J., Hook, S. C., 1990, [http://archives.datapages.com/data/bulletns/1990-91/data/pg/0074/0005/0000/0521.htm A forward modeling strategy for balancing cross sections]: AAPG Bulletin, vol. 74, p. 521–531.
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* Mount, V. S., J. Suppe, and S. C. Hook, 1990, [http://archives.datapages.com/data/bulletns/1990-91/data/pg/0074/0005/0000/0521.htm A forward modeling strategy for balancing cross sections]: AAPG Bulletin, vol. 74, p. 521–531.
* Moffat, D. T., Henage, L. F., Brash, R. A., Tauer, R. W., Harahap, B. H., 1991, Lengguru, Irian Jaya: prospect selection using field mapping, balanced cross sections, and gravity modeling: Proceedings of the Indonesian Petroleum Association's 20th Annual Convention, p. 85–106.
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* Moffat, D. T., L. F. Henage, R. A. Brash, R. W. Tauer, and B. H. Harahap, 1991, Lengguru, Irian Jaya: prospect selection using field mapping, balanced cross sections, and gravity modeling: Proceedings of the Indonesian Petroleum Association's 20th Annual Convention, p. 85–106.
* White, N., Yielding, G., 1991, [http://sp.lyellcollection.org/content/56/1/251.abstract Calculating normal faults geometries at depth: theory and examples], in Roberts, A., M., Yielding, G., Freeman, B., eds., The Geometry of Normal Faults: Geological Society of London Special Publication 56, p. 251–260.
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* White, N., and G. Yielding, 1991, [http://sp.lyellcollection.org/content/56/1/251.abstract Calculating normal faults geometries at depth: theory and examples], in Roberts, A., M., Yielding, G., Freeman, B., eds., The Geometry of Normal Faults: Geological Society of London Special Publication 56, p. 251–260.
 
* Groshong, R. H., Jr., 1990, Unique determination of normal fault shape from hanging-wall bed geometry in detached half grabens: Ecologae Geologicae Helvetiae, vol. 83, p. 455–471.
 
* Groshong, R. H., Jr., 1990, Unique determination of normal fault shape from hanging-wall bed geometry in detached half grabens: Ecologae Geologicae Helvetiae, vol. 83, p. 455–471.
 
* Gibbs, A. D., 1983, Balanced cross-section construction from seismic sections in areas of extensional tectonics: Journal of Structural Geology, vol. 5, p. 153–160, DOI: [http://www.sciencedirect.com/science/article/pii/0191814183900408 10.1016/0191-8141(83)90040-8].
 
* Gibbs, A. D., 1983, Balanced cross-section construction from seismic sections in areas of extensional tectonics: Journal of Structural Geology, vol. 5, p. 153–160, DOI: [http://www.sciencedirect.com/science/article/pii/0191814183900408 10.1016/0191-8141(83)90040-8].
* Geiser, P. A., 1988, [http://specialpapers.gsapubs.org/content/222/47.abstract The role of kinematics in the construction and analysis of [[geological cross sections<nowiki>]]</nowiki> in deformed terranes], in Mitra, G., Wojtal, S., eds., Geometries and Mechanisms of Thrusting, with Special Reference to the Appalachians: Geological Society of America Special Paper 222, p. 47–76.
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* Geiser, P. A., 1988, [http://specialpapers.gsapubs.org/content/222/47.abstract The role of kinematics in the construction and analysis of geological cross sections in deformed terranes], in G. Mitra, and S. Wojtal, eds., Geometries and Mechanisms of Thrusting, with Special Reference to the Appalachians: Geological Society of America Special Paper 222, p. 47–76.
* Diegel, V. A., Karlo, J. F., Schuster, D. C., Shoup, R. C., Tauvers, P. R., 1995, [http://archives.datapages.com/data/specpubs/memoir65/ch06/0109.htm Cenozoic structural evolution and tectono-stratigraphic framework of the northern Gulf Coast continental margin], in Jackson, M. P. A., Roberts, D. G., Snelson, S., eds., Salt Tectonics: A Global Perspective: [http://store.aapg.org/detail.aspx?id=144 AAPG Memoir 65], p. 109–151.
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* Diegel, V. A., J. F. Karlo, D. C. Schuster, R. C. Shoup, and P. R. Tauvers, 1995, [http://archives.datapages.com/data/specpubs/memoir65/ch06/0109.htm Cenozoic structural evolution and tectono-stratigraphic framework of the northern Gulf Coast continental margin], in M. P. A. Jackson, D. G. Roberts, and S. Snelson, eds., Salt Tectonics: A Global Perspective: [http://store.aapg.org/detail.aspx?id=144 AAPG Memoir 65], p. 109–151.
* Mitra, S., Namsom, J., 1989, Equal-area balancing: American Journal of Science, vol. 289, p. 563–599, DOI: [http://www.ajsonline.org/content/289/5/563.full.pdf+html 10.2475/ajs.289.5.563].
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* Mitra, S., and J. Namsom, 1989, Equal-area balancing: American Journal of Science, vol. 289, p. 563–599, DOI: [http://www.ajsonline.org/content/289/5/563.full.pdf+html 10.2475/ajs.289.5.563].
* Mitra, S., 1992, Balanced structural interpretations in fold and thrust belts, in Mitra, S., Fisher, G., W., eds., Structural Geology of Fold and Thrust Belts: Johns Hopkins University Press, Maryland, p. 53–77.
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* Mitra, S., 1992, Balanced structural interpretations in fold and thrust belts, in S. Mitra, and G. W. Fisher, eds., Structural Geology of Fold and Thrust Belts: Johns Hopkins University Press, Maryland, p. 53–77.
* Baby, P., Herail, G., Salinas, R., Sempere, T., 1992, Geometry and kinematic evolution of passive roof duplexes deduced from cross section balancing: example from the foreland thrust system of the southern Bolivian Subandean zone: Tectonics, vol. 11, p. 523–536, DOI: [http://onlinelibrary.wiley.com/doi/10.1029/91TC03090/abstract 10.1029/91TC03090].
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* Baby, P., G. Herail, R. Salinas, and T. Sempere, 1992, Geometry and kinematic evolution of passive roof duplexes deduced from cross section balancing: example from the foreland thrust system of the southern Bolivian Subandean zone: Tectonics, vol. 11, p. 523–536, DOI: [http://onlinelibrary.wiley.com/doi/10.1029/91TC03090/abstract 10.1029/91TC03090].
* Buchanan, P. G., Bishop, D. J., Hood, D. N., 1996, [http://sp.lyellcollection.org/content/100/1/111.abstract Development of salt-related structures in the central North Sea: results from section balancing], in Alsop, G. I., Blun-dell, D. J., Davison, I., eds., Salt Tectonics: Geological Society of London Special Publication 100, p. 111–128.
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* Buchanan, P. G., D. J. Bishop, and D. N. Hood, 1996, [http://sp.lyellcollection.org/content/100/1/111.abstract Development of salt-related structures in the central North Sea: results from section balancing], in G. I. Alsop, D. J. Blundell, and I. Davison, eds., Salt Tectonics: Geological Society of London Special Publication 100, p. 111–128.
* Rowan, M. G., Kligfield, R., 1989, [http://archives.datapages.com/data/bulletns/1988-89/data/pg/0073/0008/0950/0955.htm Cross section restoration and balancing as aid to seismic interpretation in extensional terranes]: AAPG Bulletin, vol. 73, p. 955–966.
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* Rowan, M. G., and R. Kligfield, 1989, [http://archives.datapages.com/data/bulletns/1988-89/data/pg/0073/0008/0950/0955.htm Cross section restoration and balancing as aid to seismic interpretation in extensional terranes]: AAPG Bulletin, vol. 73, p. 955–966.
 
* Rowan, M. G., 1993, A systematic technique for the sequential restoration of salt structures: Tectonophysics, vol. 228, p. 331–348, DOI: [http://www.sciencedirect.com/science/article/pii/004019519390347M 10.1016/0040-1951(93)90347-M].
 
* Rowan, M. G., 1993, A systematic technique for the sequential restoration of salt structures: Tectonophysics, vol. 228, p. 331–348, DOI: [http://www.sciencedirect.com/science/article/pii/004019519390347M 10.1016/0040-1951(93)90347-M].
* Marshak, S., Woodward, N., 1988, Introduction to cross-section balancing in Marshak, S., Mitra, G., eds., Basic Methods of Structural Geology: Englewood Cliffs, New Jersey, Prentice Hall, p. 303–302.
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* Marshak, S., and N. Woodward, 1988, Introduction to cross-section balancing in Marshak, S., Mitra, G., eds., Basic Methods of Structural Geology: Englewood Cliffs, New Jersey, Prentice Hall, p. 303–302.
* Hossack, J., 1995, [http://archives.datapages.com/data/specpubs/memoir65/ch02/0029.htm Geometric rules of section balancing for salt structures], in Jackson, M., P., A., Roberts, D., G., Snelson, S., eds., Salt Tectonics: A Global Perspective: [http://store.aapg.org/detail.aspx?id=144 AAPG Memoir 65], p. 29–40.
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* Hossack, J., 1995, [http://archives.datapages.com/data/specpubs/memoir65/ch02/0029.htm Geometric rules of section balancing for salt structures], in M. P. A. Jackson, D. G. Roberts, and S. Snelson, eds., Salt Tectonics: A Global Perspective: [http://store.aapg.org/detail.aspx?id=144 AAPG Memoir 65], p. 29–40.
* Rouby, D., Fossen, H., Cobbold, P. R., 1996, [http://archives.datapages.com/data/bulletns/1994-96/data/pg/0080/0006/0850/0875.htm Extension, displacement, and block rotation in the larger Gullfaks area, northern North Sea: determined from map view restoration]: AAPG Bulletin, vol. 80, p. 875–890.
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* Rouby, D., H. Fossen, P. R. Cobbold, 1996, [http://archives.datapages.com/data/bulletns/1994-96/data/pg/0080/0006/0850/0875.htm Extension, displacement, and block rotation in the larger Gullfaks area, northern North Sea: determined from map view restoration]: AAPG Bulletin, vol. 80, p. 875–890.
  
 
==See also==
 
==See also==
* [[Prospect delineation techniques and tools]]
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* [[Seismic data]]
 
* [[Seismic data]]
 
* [[Tectonic modeling]]
 
* [[Tectonic modeling]]
* [[Dipmeter analysis]]
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* [[Dipmeter]]
 
* [[Petrofabrics]]
 
* [[Petrofabrics]]
 
* [[Fracture analysis]]
 
* [[Fracture analysis]]
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[[Category:Predicting the occurrence of oil and gas traps]]  
 
[[Category:Predicting the occurrence of oil and gas traps]]  
 
[[Category:Exploring for structural traps]]
 
[[Category:Exploring for structural traps]]
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[[Category:Treatise Handbook 3]]

Latest revision as of 15:07, 3 February 2022

Exploring for Oil and Gas Traps
Series Treatise in Petroleum Geology
Part Predicting the occurrence of oil and gas traps
Chapter Exploring for structural traps
Author R.A. Nelson, T.L. Patton, S. Serra
Link Web page
Store AAPG Store

Definition

Balanced cross sections honor all available data and are constructed and analyzed to ensure they are geometrically possible and geologically admissible, given reasonable assumptions about the predeformation setting of rocks and how rocks behave during deformation in a particular tectonic environment. “Balanced” refers to the basic assumption made in constructing these sections—that rock area (rock volume) does not change substantially as a result of deformation. Balanced cross sections are restorable. This means that, while maintaining constant area, the deformation displayed in a balanced cross section can be incrementally removed to yield a geologically plausible predeformation configuration.

The constant area (constant volume) assumption is generally valid for deformation that has occurred in upper crustal, nonmetamorphic settings, but there are important exceptions. For example, in some settings syntectonic deposition and compaction can result in substantial rock volume changes throughout the course of deformation. In these cases, approximations of the volume changes must be incorporated in the balancing process.

Balancing is an interative, trial-and-error process. If done manually, it is tedious and very time consuming. Computer programs greatly simplify the measurement and drafting aspects of cross section balancing. Some of these programs also incorporate functions and algorithms that permit some rudimentary 3-D balancing of structures.

Value of balancing

Balanced cross sections are not necessarily correct. However, the methodical scrutiny imposed by the balancing process highlights discrepancies in interpretations, points to the types of data or alternative schemes needed to resolve the discrepancies, and generally results in more carefully constructed, defensible, and explainable cross sections.

Further reading

Examples of use

See also

External links

find literature about
Balanced cross sections
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