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Carbonates and Evaporites

, Volume 9, Issue 2, pp 143–150 | Cite as

Upper Cambrian-Lower Ordovician (Sauk) platform carbonates of the northern Appalachian (Gondwana) passive margin

  • Gerald M. Friedman
Article

Abstract

Sauk platform carbonates of the northern Appalachian passive (Gondwana) margin are composed of high-frequency stacking patterns containing fifth-order depositional cycles. Most of the these cycles, termed parasequences in this study, display upward-shoaling peritidal patterns, commonly terminating in emergence. Parasequence surfaces are erosional resulting from this emergence and have associated karst features, especially solution-collapse breaccia. The carbonates, mostly fine- to medium-crystalline and locally vuggy dolostones, are generally of low permeability. Solution-collapse breccias increase whole-rock permeability through fractures. In addition to solution-collapse breccias, emergence generated terra-rossa soil, now lithified, as well as silcrete, now chert, and caused the dedolomitization of dolostones.

Upward-coarsening facies cycles, in which flat-pebble conglomerates overlie erosional surfaces, are thought to be storm generated. Yet storm deposits with intraclasts sufficiently angular to be termed breccia may also terminate parasequences.

Fifth-order upward-shoaling peritidal parasequences may be the result of extraterrestrial forcing or tectonic events causing rapid eustatic or relative changes in sea-level, respectively. Hence porosity-permeability development may likewise relate to these mechanisms. During the Sauk interval anomalous storm periods may have held sway on a global scale and generated upward-coarsening parasequences. Storm-weather periods probably resulted from astronomical changes (extraterrestrial forcing). Porosity and permeability in the storm deposits may also be controlled by extraterrestrial forcing functions.

Keywords

Cambrian Breccia Ordovician Stromatolite Micrite 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. AMTHOR, J.E., and FRIEDMAN, G.M., 1992, Early-to-late-diagenetic dolomitization of platform carbonates: Lower Ordovician Ellenberger Group, Permian Basin, west Texas:Jour. Sedimentary Petrology, v. 62, p. 131–144.Google Scholar
  2. ANDERSON, W.H., 1991, Mineralization and hydrocarbon emplacement in the Cambrian-Ordovician Mascot Dolomite of the Knox Group in south-central Kentucky, Kentucky Geol. Survey Report of Investigations, No. 4, 31 p.Google Scholar
  3. BOND, G.C., NICKERSON, P.A., and KOMINZ, M.A., 1984, Breakup of a supercontinent between 625 Ma and 555 Ma: new evidence and implications for continental histories:Earth and Planetary Science Letters, v. 70, p. 325–345.CrossRefGoogle Scholar
  4. CHOW, N., and JAMES, N.P., 1987, Cambrian Grand Cycles: a northern Appalachian perspective,Geological Society of America Bulletin, v. 98, p. 418–429.CrossRefGoogle Scholar
  5. CHUANMAO, Liang, FRIEDMAN, G.M., and SANDERS, J.E., 1992, Petrofacies and petrophysical analysis of parts of Sauk Sequence carbonates (Upper Cambrian-Lower Ordovician): Parts of Briarcliff and Pine Plains formations (Wappinger Group), Dutchess County, North Central Appalachians, Southeastern New York State:Northeastern Geology, v. 14, p. 44–58.Google Scholar
  6. CHUANMAO, Liang, FRIEDMAN, G.M., and ZHAOCHANG, Zheng, 1993, Carbonate storm deposits (tempestites) of Middle to Upper Cambrian age in the Helen Mountains, northwest China:Carbonates and Evaporites, v. 8, p. 181–190.CrossRefGoogle Scholar
  7. CURL, M.W., ZAGORSKI, T.W., and FRIEDMAN, G.M., 1984, Depositional environments and diagenesis of subsurface Tribes Hill Formation (Lower Ordovician), Mohawk Valley, New York:The Compass, v. 61, p. 216–243.Google Scholar
  8. DEMICCO, R.V., 1985, Patterns of platform and offplatform carbonates of the Upper Cambrian of western Maryland,Sedimentology, v. 32, p. 1–22.CrossRefGoogle Scholar
  9. DYKSTRA, J.C.F., 1992, Drilling for deep gas in Quebec:Northeastern Geology, v. 14, p. 65–66.Google Scholar
  10. ERVILUS, PA., and FRIEDMAN, G.M., 1991, Note on Cambro-Ordovician dolostones (the Pine Plains Formation) in southern New York:Northeastern Geology, v. 13, p. 165–176.Google Scholar
  11. FRIEDMAN, G.M., 1964, Early diagenesis and lithification in carbonate sediments:Journal of Sedimentary Petrology, v. 34, p. 777–813.Google Scholar
  12. FRIEDMAN, G.M., and SANDERS, J.E., 1967, Origin and occurrence of dolostones, p. 267–348in Chilingar, G.V., Bissell, H.J., and Fairbridge, R.W., (eds.), Carbonate rocks, origin, occurrence, and classification, Amsterdam, London, New York, Elsevier Publishing Company, 471 p.CrossRefGoogle Scholar
  13. FRIEDMAN, G.M., and SANDERS, J.E., 1978, Principles of sedimentology. New York, John Wiley & Sons, 792 p.Google Scholar
  14. FRIEDMAN, G.M., and RADKE, Bruce, 1979, Evidence for sabkha overprint and conditions of intermittent emergence in Cambrian-Ordovician carbonates of northeastern North America and Queensland, Australia:Northeastern Geology, v. 1, p. 18–42.Google Scholar
  15. FRIEDMAN, G.M., SANDERS, J.E., and GUO, Baiying, 1992, Pre-drilling geologic work in connection with proposed Albany Basin, New York, deep scientific bore hole to test gas potential of Paleozoic formations, Monthly Progress Report, New York Gas Group. December. 1992, 11 p.Google Scholar
  16. FRIEDMAN, G..M., SANDERS. J.E., and GUO, Baiying, 1993, Pre-drilling geologic work in connection with proposed Albany Basin, New York, deep scientific bore hole to test gas potential of Paleozoic formations: Final Report, New York Gas Group, 167 p.Google Scholar
  17. FRIEDMAN, G.M., SANDERS, J.E., and KOPASKA-MERKEL, D.C., 1992, Principles of sedimentary deposits: stratigraphy and sedimentology: New York, Macmillan Publ. Co., 717 p.Google Scholar
  18. GOLDHAMMER, R.K., LEHMANN, P.J., and DUNN, PA., 1993, The origin of high-frequency platform carbonate cycles and third-order sequences (Lower Ordovician El Paso Gp, West Texas): Constraints from outcrop data and stratigraphic modelling:Journal of Sedimentary Petrology, v. 63, p. 318–359.Google Scholar
  19. GOODING, P.J., 1992, Unconformity at the top of the Knox Group (Cambrian and Ordovician) in the subsurface of south-central Kentucky. Kentucky Geol. Survey, Thesis Series 4, 40 p.Google Scholar
  20. GREINER, G.F., 1982, Geology of a regressive peritidal sequence with evaporitic overprints: the subsurface Dunham Formation (Lower Cambrian), Franklin, Vermont, unpubl. Master’s thesis, Rensselaer Polytechnic Institute, 116 p.Google Scholar
  21. GUO, Baiying, 1994, Diagenesis: cementation, dolomitization, and dedolomitization, including petrophysical characteristics of carbonate rocks, unpubl. Ph.D. thesis, City University of New York.Google Scholar
  22. HARRIS, R.L., and FRIEDMAN, G.M., 1982, Depositional environments of the subsurface Ogdensburg, Formation (Lower Ordovician) in northern New York State:Northeastern Geology, v. 4, p. 151–166.Google Scholar
  23. KERANS, Charles, HOLT, M.H., and TYLER, Noel, 1989, Contrasting styles of reservoir heterogeneity in Ellenburger Group carbonates, West Texas,in Cunningham, B.K., and Cromwell, W., (eds.), The Lower Paleozoic of West Texas and Southern New Mexico: modern exploration concepts:Permian Basin Section, Soc. Economic Paleont. Min., v. 31, p. 131.Google Scholar
  24. KOERSCHNER, W.F., and READ, J.F., 1989, Field and modelling studies of Cambrian carbonate cycles, Virginia Appalachians:Journal of Sedimentary Petrology, v. 59, p. 654–687.Google Scholar
  25. LOGAN, B.W., 1961,Cryptozoan and associated stromatolites from the Recent, Shark Bay, western Australia:Journal of Geology, v. 69, p. 517–533.CrossRefGoogle Scholar
  26. LOUCKS, R.G., and HANDFORD, C.R., 1992, Origin and recognition of fractures, breccias, and sediment fills in paleocave-reservoir networks,in Candelaria, M.P. and Reed, C.L., (eds.), Paleokarst, Karst-Related Diagenesis, and Reservoir Development Examples from Ordovician- Devonian Age Strata of West Texas and the Mid-Continent, 1992 Field Trip Guidebook, Permian Basin Section SEPM (Society for Sedimentary Geology), p. 31–44.Google Scholar
  27. MAZZULO, S.J., and FRIEDMAN, G.M., 1975, Conceptual model of tidally influenced deposition on margins of epeiric seas: Ordovician (Canadian) of eastern New York and southwestern Vermont:Bulletin of American Association of Petroleum Geologists, v. 59, p. 2123–2141.Google Scholar
  28. MONTAÑEZ, I.P., and READ, J.F., 1992, Fluid-rock interaction history during stabilization of early dolomites, Upper Knox Group (Lower Ordovician), U.S. Appalachians:Journal of Sedimentary Petrology, v. 62, p. 753–778.Google Scholar
  29. NORTON, W.H., 1917, A classification of breccias:Journal of Geology, v. 25, p. 160–194.CrossRefGoogle Scholar
  30. PHILLIPS. S.E., and SELF, P.G., 1987, Morphology, crystallography, and origin of needle-fibre calcite in Quarternary pedogenic calcretes of South Australia:Australian Jour. Soil Research, v. 25, p. 249–264.Google Scholar
  31. RADKE, B.M., 1978, Carbonate sedimentation in tidal and epeiric environments and diagenetic overprints: the Ninmaroo Formation (Upper Cambrian-Lower Ordovician), Central Australia. unpubl. Ph.D. thesis, Rensselaer Polytechnic Institute, 254 p.Google Scholar
  32. RADKE, B.M., and DUFF, P., 1980, A potential dolostone reservoir in the Georgina Basin: the Lower Ordovician Kelly Creek Formation:BMR Jour. Australian Geology and Geophysics, v. 5, p. 160–163.Google Scholar
  33. RUBIN, D.M., and FRIEDMAN, G.M., 1981, Origin of chert grains and a halite-silcrete bed in the Cambrian and Ordovician Whitehall Formation of eastern New York State:Journal of Sedimentary Petrology, v. 51, p. 69–72.Google Scholar
  34. SARWAR, Golam, and FRIEDMAN, G..M., 1994, Late Paleozoic sediment cover on the Adirondacks, New York: evidence from fluid inclusions and clay diagenesis:Northeastern Geology, v. 16, p. 19–37.Google Scholar
  35. SHEARMAN, D.J., KHOURI, J., and TAMA, S., 1961, On the replacement of dolomite by calcite in some Mesozoic limestones from the French Jura:Geologists’ Association (London) Proceedings, v. 72, p. 1–12.CrossRefGoogle Scholar
  36. THERIAULT, F., and HUTCHEON, I., 1987, Dolomitization of the Devonian Grosmont Formation, northern Alberta:Journal of Sedimentary Petrology, v. 57, p. 955–966.Google Scholar
  37. TURMELLE, J.M., 1993, Heluma and King Mountain Fields backthrusted structures, Upton County, Texas:Bull. Houston Geol. Soc., v. 35, No. 8, p. 22–49.Google Scholar
  38. VAN WAGONER, J.C., 1985, Reservoir facies distribution as controlled by sea-level change. Soc. Economic Paleontologists and Mineralogists Mid-Year Meeting, Abstract and Poster Session, p. 91–92.Google Scholar
  39. WILSON, J.L., 1952, Upper Cambrian stratigraphy in the Central Appalachians:Geological Society of America Bulletin, v. 63, p. 275–322.CrossRefGoogle Scholar

Copyright information

© Springer 1994

Authors and Affiliations

  • Gerald M. Friedman
    • 1
    • 2
  1. 1.Brooklyn College and Graduate School of the City University of New YorkBrooklyn
  2. 2.Rensselaer Center of Applied GeologyNortheastern Science Foundation, affiliated with Brooklyn CollegeTroy

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