Structural interpretation and restoration of Rocky Mountain Brazeau zone

Juhee Kang, Heejung Kim

Journal of Earth Science ›› 2017, Vol. 28 ›› Issue (5) : 867-873.

Journal of Earth Science ›› 2017, Vol. 28 ›› Issue (5) : 867-873. DOI: 10.1007/s12583-017-0775-z
Articles

Structural interpretation and restoration of Rocky Mountain Brazeau zone

Author information +
History +

Abstract

The Rocky Mountain Foothills lie along the eastern margin of the Rocky Mountain fold-thrust belt. The area has been the focus of extensive research aimed at locating oil and gas fields with the potential to be used as CO2 storage traps. In this study, we use a seismic line from the Canadian Rockies to interpret the geologic structures along a cross-section parallel to the tectonic transport direction. We then compare our results with those of previous studies. The section was restored using the MOVE software (manufactured by Midland Valley Exploration Ltd.). The primary objectives of this work are: (1) to conduct a stratigraphic and structural interpretation of a 2D seismic profile; and (2) to conduct a cross-sectional restoration of the structures in order to validate the seismic interpretation in terms of CO2 storage candidates. Additional data sources include maps of the surface geology, which show that the age of horizons decrease from west to east, and stratigraphic and structural profiles derived from well logs. The results of our structural restoration indicate a detachment fault between the foreland and hinterland. This fault is responsible for the cutting and subsequent upwards and eastwards movement of a stratum located between the basement and the Late Devonian formation. Large thrust faults are responsible for the deformation of strata (through both folding and faulting) in the foreland basin. As a result of continuous eastward tectonic stress, the strata from Jurassic have deformed, forming a duplex system in the middle of the section and resulting in the uplift of the upper part of the section. Following surface erosion, this uplifted area became exposed during the Tertiary Period. The high shortening rate (53%) detected through structural restoration is consistent with the thin-skinned tectonic model.

Keywords

Rocky Mountain Foothills / fold-thrust belt / stratigraphic and structural interpretation / structural restoration

Cite this article

Download citation ▾
Juhee Kang, Heejung Kim. Structural interpretation and restoration of Rocky Mountain Brazeau zone. Journal of Earth Science, 2017, 28(5): 867‒873 https://doi.org/10.1007/s12583-017-0775-z

References

Bally A. W., Gordy P. L., Stewart G. A. Structural Seismic Data and Orogenic Evolution of Southern Canadian Rocky Mountain. Bulletin of Canadian Petroleum Geology, 1966, 14: 337-381.
Boyer S. E., Elliott D. Thrust Systems. American Association of Petroleum Geologists Bulletin, 1982, 66: 1196-1230.
Brandes C., Tanner D. C. Fault-Related Folding: A Review of Kinematic Models and Their Application. Earth-Science Reviews, 2014, 138: 352-370.
CrossRef Google scholar
Cooley M. A., Price R. A., Kyser T. K., . Stable-Isotope Geochemistry of Syntectonic Veins in Paleozoic Carbonate Rocks in the Livingstone Range Anticlinorium and Their Significance to the Thermal and Fluid Evolution of the Southern Canadian Foreland Thrust and Fold Belt. AAPG Bulletin, 2011, 95(11): 1851-1882.
CrossRef Google scholar
Covault J. A., Buursink M. L., Craddock W. H., . Geologic Framework for the National Assessment of Carbon Dioxide Storage Resources-Bighorn Basin, Wyoming and Montana, 2012.
Dahlstrom C. D. A. Balanced Cross Sections. Canadian Journal of Earth Sciences, 1969, 6(4): 743-757.
CrossRef Google scholar
Dahlstrom C. D. A. Structural Geology in Eastern Margin of Canadian Rocky Mountains. Bulletin of Canadian Petroleum Geology, 1970, 18(3): 322-340.
Elliott D. The Construction of Balanced Cross-Sections. Journal of Structural Geology, 1983, 5 2 101
CrossRef Google scholar
Elliott D., Johnson M. R. W. Structural Evolution in the Northern Part of the Moine Thrust Belt, NW Scotland. Transactions of the Royal Society of Edinburgh: Earth Sciences, 1980, 71(2): 69-96.
CrossRef Google scholar
Gunther P. R., Hills L. V. Megaspores and Other Palynomorphs of the Brazeau Formation (Upper Cretaceous), Nordegg Area, Alberta. Geoscience and Man, 1972, 4(1): 29-48.
CrossRef Google scholar
Price R. A. de Jong K. A., Scholten R. Large-Scale Gravitational Flow of Supracrustal Rocks, Southern Canadian Rockies. Gravity and Tectonics, 1973, New York: John Wiley and Sons, 491-502.
Price R. A., Mountjoy E. W. Geologic Structure of the Canadian Rocky Mountains between Bow and Athabasca Rivers: A Progress Report. In: Wheeler, J. O., ed., Structture of the Southern Canadian Cordillera. Geological Association of Canada Special Publication, 1970, 6: 7-25.
Ranganai R. T., Whaler K. A., Ebinger C. J. Aeromagnetic Interpretation in the South-Central Zimbabwe Craton: (Reappraisal of) Crustal Structure and Tectonic Implications. International Journal of Earth Sciences, 2015, 105(8): 2175-2201.
CrossRef Google scholar
Roure F., Swennen R., Schneider F., . Incidence and Importance of Tectonics and Natural Fluid Migration on Reservoir Evolution in Foreland Fold-and-Thrust Belts. Oil & Gas Science and Technology, 2005, 60(1): 67-106.
CrossRef Google scholar
Sclater J. G., Christie P. A. F. Continental Stretching: An Explanation of the Post-Mid-Cretaceous Subsidence of the Central North Sea Basin. Journal of Geophysical Research: Solid Earth, 1980, 85(B7): 3711-3739.
CrossRef Google scholar
Smith D. G. Mossop G. D., Shetsen I. Paleogeographic Evolution of the Western Canada Foreland Basin. The Geological Atlas of the Western Canada Sedimentary Basin, 1994, Calgary: Canadian Society of Petroleum Geologists and Alberta Research Council, 277-295.
Stott D. F. Lower Cretaceous Fort St. John Group and Upper Cretaceous Dunvegan Formation of the Foothills and Plains of Alberta, British Columbia, District of Mackenzie and Yukon Territory. Geological Survey of Canada, Bulletin, 1982, 328 124.
Suppe J. Geometry and Kinematics of Fault-Bend Folding. American Journal of Science, 1983, 283(7): 684-721.
CrossRef Google scholar
Taerum R. L. Effect of Mechanical Stratigraphy on Structural Style Variations in the Central Alberta Fold and Thrust Belt: [Dissertation], 2011, Calgary: University of Calgary, 228.
van der Pluijm B. A., Vrolijk P. J., Pevear D. R., . Fault Dating in the Canadian Rocky Mountains: Evidence for Late Cretaceous and Early Eocene Orogenic Pulses. Geology, 2006, 34(10): 837-840.
CrossRef Google scholar
Woodward N., Boyer S. E., Suppe J. Balanced Geological Cross-Sections: An Essential Technique in Geological Research and Exploration. American Geophysical Union Short Course in Geology, 1989, 6 132.

Accesses

Citations

Detail

Sections
Recommended

/