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Showing 1 to 3 of 3 for “"siliclastics"”.

  1. Evolution of early Proterozoic passive-margin carbonate platform, Rocknest Formation, Wopmay Orogen, N.W.T., Canada

    … cyclic facies pass eastward into non—cyclic siliclastics of central and eastern "lagoon". The shelf was terminally drovmed during attempted subduction of the margin. Individual cycles are correlatable for over 200 km parallel to strike and over 120 Ion perpendicular to strike. Cycles formed …

    vt Repository record for Evolution of early Proterozoic passive-margin carbonate platform, Rocknest Formation, Wopmay Orogen, N.W.T., Canada (opens in a new tab)

  2. Fayetteville and Imo Shales: Punctuated Upper Mississippian Shallowing Upward Sequence, Southern Ozark Region, Northern Arkansas

    … unconformably by Pennsylvanian (Morrowan) siliclastics of the Hale Formation (Stevens and Manger, 2018).</p> <p>The carbonaceous black fissile shales of both the Fayetteville Shale and Pitkin Limestone, Imo Member, were originally thought to have been deposited in deep water basinal …

    arkansas Repository record for Fayetteville and Imo Shales: Punctuated Upper Mississippian Shallowing Upward Sequence, Southern Ozark Region, Northern Arkansas (opens in a new tab)

  3. Sequence Stratigraphy of the Bridal Veil Falls Limestone, Carboniferous, Lower Oquirrh Group, on Cascade Mountain, Utah: A standard Morrowan Cyclostratigraphy for the Oquirrh Basin

    The Bridal Veil Falls Limestone (lowest 400 meters of the Permo-Carboniferous Oquirrh Group) is well exposed on the flanks of Cascade Mountain (Wasatch Front and adjacent mountain ranges) near Provo, Utah. Because of its excellent exposure and location in the heart of the Oquirrh depocenter, this …

    byu Repository record for Sequence Stratigraphy of the Bridal Veil Falls Limestone, Carboniferous, Lower Oquirrh Group, on Cascade Mountain, Utah: A standard Morrowan Cyclostratigraphy for the Oquirrh Basin (opens in a new tab)