DGGS AOF 114
Tertiary formations in the Kodiak Island area, Alaska, and their petroleum reservoir and source-rock potential
Authors:
Lyle, W.M., Morehouse, J.A., Palmer, I.F., Jr., Bolm, J.G., Moore, G.W., and Nilsen, T.H.
Publication Date:
1978
Publisher:
Alaska Division of Geological & Geophysical Surveys
Comments:
These scanned images may difficult to decipher due to the condition and image quality limitations of the original file. Mylar originals are archived in the DGGS technical library and are available for in-house viewing. AGDI catalog number 34484
Ordering Info:
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Quadrangle(s):
Kaguyak; Kodiak; Trinity Islands
Citation ID:
30
Bibliographic Reference
Lyle, W.M., Morehouse, J.A., Palmer, I.F., Jr., Bolm, J.G., Moore, G.W., and Nilsen, T.H., 1978, Tertiary formations in the Kodiak Island area, Alaska, and their petroleum reservoir and source-rock potential: Alaska Division of Geological & Geophysical Surveys Alaska Open-File Report 114, 59 p., 10 sheets. https://doi.org/10.14509/30
Publication Products
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Report Information
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Maps & Other Oversized Sheets
- Plate A, Kodiak Quadrangle - sample locations, scale 1:250,000 (8.0 M)
- Plate B, Trinity Islands Quadrangle - sample locations, scale 1:250,000 (2.2 M)
- Plate C, Kaguyak Quadrangle - sample locations, scale 1:250,000 (2.0 M)
- Plate I, Geese Island stratigraphic section, scale 1 inch = 60 feet (9.8 M)
- Plate II, McDonald Lagoon stratigraphic section segments, scale 1 inch = 100 feet (1.1 M)
- Plate III, Narrow Cape stratigraphic section, scale 1 inch = 50 feet (26.0 M)
- Plate IV, Ocean Bay stratigraphic section, scale 1 inch = 60 feet (12.0 M)
- Plate V, Partition Cove stratigraphic section, scale 1 inch = 60 feet (8.9 M)
- Plate VI, Sitkinak stratigraphic section, scale 1 inch = 100 feet (29.0 M)
- Plate VII, Twoheaded Island stratigraphic section, scale 1 inch = 50 feet (25.0 M)
Keywords
Depositional Environment; Geochemistry; Paleobotany; Paleontology; Petrography; Petroleum; Reservoir Model; Resource Assessment; Stratigraphy; Stream Sediments; Tertiary
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