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Magnetostratigraphy and paleopoles of the Kayenta Formation and the Tenney Canyon Tongue

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Treść / Zawartość
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The Kayenta Formation is the third in a series of stratigraphic units making up the Glen Canyon Group that were sampled along US Hwy 89 in southern Utah. The Kayenta is dominantly reversed polarity with a number of very short normal polarity intervals. Above the Kayenta and interbedded in the Navajo Sandstone is the Tenney Canyon Tongue of the Kayenta Formation. The lower half of the Tenney Canyon Tongue was also sampled and is dominantly normal polarity with three short reversed polarity intervals. The dominantly reversed magnetostratigraphy of the Kayenta appears to match that of Early Pliensbachian polarity interval “e-Pli R.” The dominance of normal polarity of the Tenney Canyon Tongue suggests that the Tenney Canyon may have been deposited in the upper half of the Pliensbachian polarity interval “ePli-N.” The suggested polarity matches indicate that the Kayenta and Tenney Canyon Tongue strata are 187–190 Ma in age. The paleopoles of the two units are statistically identical. The combined data of the Kayenta-Springdale-Whitmore Point show that the J-1 cusp terminated before the deposition of the Kayenta Formation. The North American continent/pole returned to its Late Triassic position during/after Springdale time, apparently along the same path used to reach the apex of the J-1 cusp.
Czasopismo
Rocznik
Strony
31--38
Opis fizyczny
Bibliogr. 12 poz.
Twórcy
autor
  • Department of Geology and Geophysics, University of Wyoming, Laramie, Wyoming, 82071, USA
autor
  • Environmental Science Systems, Le Moyne College, Syracuse New York, 13214, USA
Bibliografia
  • 1.Bazard D.R., Butler R.F., 1991 — Paleomagnetism of the Chinle and Kayenta Formations, New Mexico and Arizona. Journal of Geophysical Research, 96: 9847–9871.
  • 2.Clark J.M., Fasto vsky D.E., 1986—Vertebrate biostratigraphy of the Glen Canyon Group in northern Arizona. In: The beginning of the age of the dinosaurs (Ed. K. Padian): 285–301. Cambridge University Press.
  • 3.Gradstein F.M., Ogg J.G., Schmidt M.D., Ogg G.M., 2012— The Geologic Time Scale, Vol. 2. Elsevier BV, Amsterdam.
  • 4.Kirschvink J., 1980 — The least-squares line and plane and the analysis of palaeomagnetic data. Geophysical Journal, 62: 699–718.
  • 5.Lucas S.G., Tanner L.H., 2006 — The Springdale Member of the Kayenta Formation, Lower Jurassic of Utah-Arizona. New Mexico Museum of Natural History and Science Bulletin, 37: 71–76.
  • 6.Milner A.R.C., Kirkland J.I., Birthisel T.A., 2006 —The geographic distribution and biostratigraphy of Late Triassic-Early Jurassic freshwater fish faunas of the Southwestern United States. New Mexico Museum of Natural History and Science Bulletin, 37: 522–529.
  • 7.Moreau M.-G., Bucher H., Bodergat A.-M., Guex J., 2002 — Pliensbachian magnetostratigraphy: new data from the Paris Basin (France). Earth and Planetary Science Letters, 203: 755–767.
  • 8.Padian K., 1989 — Presence of the dinosaur Scelidosaurus indicates Jurassic age for the Kayenta Formation (Glen Canyon Group, northern Arizona). Geology, 17: 438–441.
  • 9.STEINER M., 2014a — New magnetostratigraphy and paleopole from the Whitmore Point Member of the Moenave Formation at Kanab, Utah. Volumina Jurassica, 12, 2: 13–22 (this volume).
  • 10.STEINER M., 2014b — Age of Lower Jurassic Springdale Sandstone of Southwestern Utah from its magnetic polarity sequence. Volumina Jurassica, 12, 2:23–30 (this volume).
  • 11.Steiner M.B., Lucas S.G., 2000 — Paleomagnetism of the Late Triassic Petrified Forest Formation, Chinle Group, western United States: Further evidence of “large” rotation of the Colorado Plateau. Journal of Geophysical Research, 105: 25791–25808.
  • 12.Steiner M.B., Helsley C.E., 1974 — Magnetic polarity of the Kayenta Formation near Moab, UT. Geology, 2: 191–194
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-c66a4113-b839-484f-85b2-1e3a608984f8
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