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National Geologic Map Database
Geologic Unit: Kemik
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Map showing publication footprint
  • Usage in publication:
    • Kemik sandstone member*
  • Modifications:
    • Named
  • Dominant lithology:
    • Sandstone
  • AAPG geologic province:
    • Alaska Northern region
Publication:

Keller, A.S., Morris, R.H., and Detterman, R.L., 1961, Geology of the Shaviovik and Sagavanirktok Rivers region. Alaska, IN Exploration of Naval Petroleum Reserve No. 4 and adjacent areas, northern Alaska, 1944-53; Part 3, Areal geology: U.S. Geological Survey Professional Paper, 303-D, p. D169-D222, (incl. geologic map, scale 1:125,000)


Summary:

Named as basal member of Okpikruak formation. Measured type section is on east side of Kemik Creek between 69 deg 24'N and 69 deg 25'N. Extends from Echooka River to Kavik River. Forms faulted rubble ridges and apparently pinches out both to west and east. Composed of quartzose fine- to medium-grained, sugary-textured light-gray sandstone. Is 220 ft thick at type. Overlies Jurassic shale. Fossils collected from unit are not age diagnostic but age of member is considered to be Early Cretaceous based on age of Okpikruak formation.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Kemik Sandstone Member*
  • Modifications:
    • Revised
  • AAPG geologic province:
    • Alaska Northern region
Publication:

Detterman, R.L., Reiser, H.N., Brosge, W.P., and Dutro, J.T., Jr., 1975, Post-Carboniferous stratigraphy, northeastern Alaska: U.S. Geological Survey Professional Paper, 886, 46 p.


Summary:

Rocks of Okpikruak Formation in northeast AK are renamed Kongakut Formation because lithology is dissimilar to that of Okpikruak in its type locality. Kemik Sandstone member is reassigned to Kongakut Formation. Sandstone along west side of Canning River near Shublik Springs considered by Keller and others (1961) to be lower part of Ignek Formation is here considered to be Kemik Sandstone member (Ignek Formation is abandoned). At type section of Kongakut, north of Bathtub Ridge, Kemik Sandstone Member overlies clay shale member and underlies pebble shale member (both of Kongakut Formation). Upper part of Kemik Sandstone Member contains sparse megafauna of Early Cretaceous age.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Kemik Sandstone*
  • Modifications:
    • Revised
  • AAPG geologic province:
    • Alaska Northern region
Publication:

Molenaar, C.M., Bird, K.J., and Kirk, A.R., 1987, Cretaceous and Tertiary stratigraphy of northeastern Alaska, IN Tailleur, I.L., and Weimer, Paul, eds., Alaskan North Slope geology; Volume 1: Society of Economic Paleontologists and Mineralogists, Pacific Section, North Slope Seminar II, AAPG/SEPM/SEG Pacific Section annual meeting, Anchorage, AK, May 22-24, 1985, book 50, p. 513-528., Prepared by SEPM Pacific Section and Alaska Geol. Soc


Summary:

Kemik Sandstone Member raised to: Kemik Sandstone in area "along the mountain front and coastal plain" (area around Sadlerochit Mountains and in a southwesterly band along the Brooks Range foothills and coastal plain as far as the Echooka River, 40 mi southwest of Sadlerochit Mountains). Also occurs in several wells along the foothills as far as 70 mi west of the Canning River. Unconformably overlies progressively older units from south to north. [Still known as Kemik Sandstone member ONLY in the Bathtub Ridge area 60 mi southeast of Sadlerochit Mountains.] Unit age is Early Cretaceous (Hauterivian).

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Kemik Sandstone
  • Modifications:
    • Revised
    • Overview
  • AAPG geologic province:
    • Alaska Northern region
Publication:

Mull, C.G., 1987, Kemik Sandstone, Arctic National Wildlife Refuge, northeastern Alaska, IN Tailleur, I.L., and Weimer, Paul, eds., Alaskan North Slope geology; Volume 1: Society of Economic Paleontologists and Mineralogists, Pacific Section, North Slope Seminar II, AAPG/SEPM/SEG Pacific Section annual meeting, Anchorage, AK, May 22-24, 1985, book 50, p. 405-431., Prepared by SEPM Pacific Section and Alaska Geol. Soc


Summary:

Kemik Sandstone (redefined as formational unit) on north side of Brooks Range includes two new named members, Ignek Valley (cross-bedded sandstone) and Marsh Creek (burrowed pebbly siltstone) Members and unnamed mudstone and shale facies. Detailed lithology, stratigraphic columns and cross sections, fossil lists with localities, depositional environment ... included in report.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


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