Sample: |
Sample No. 92AD35C-15.5 -- USGS No. 32442-PC
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Locality: |
Field No. 92AD35C-15.5
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Description: |
Howard Pass B-3. Lat. 68o 20'00" N., Long. 157o 44'35" W. Sample from 80 x 45 cm concretion of fine-grained, sooty, fetid, black, medium-gray-weathering limestone (calcified radiolarite?). Thin section is calcareous radiolarian packstone; radiolarian tests (50-80 percent of slide; replaced and filled with polycrystalline calcite) and lesser calcareous sponge spicules in a matrix of brown, fine-crystalline calcite. Collected from 15.5 m above base of approx. 68 m-thick section of Kuna Formation at type locality (as designated in Mull and others, 1982); section is mostly silicified mudstone and <10 percent limestone. (description from Dover et al., 2004, p. 49 (Table 1)); [Howard Pass B-3. 68°20'00', 157°44'30". 80 x 40 cm concretion of fine-grained, sooty, fetid, black, medium gray-weathering limestone (calcified radiolarite?). Collected from 15.5 m above base ~68 m-thick type section of Kuna Fm. which is mostly silicified mudstone and <10% limestone. Collected at ~800 m elevation, ~ 1/4 mile west of 92AD35A section on north side of small tributary to Safari Creek, ~1 mile southeast of hill 950 m and ~2.75 miles due west of headwaters of Ipnavik River, NW1/4 sec. 21, T. 34 N., R. 5 E. (description from Harris E&R report dated March 17, 1995)] |
Location: |
Alaska Quadrangle: Howard Pass B-3 Township&Range: 34 N. 5 E. Section: 21 Lat.: 68o20'00 " Long.: 157o44'35 " |
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Reference
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Title: |
Report on Referred Fossils
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1995
(03/17)
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Analysis of all samples is given in the accompanying 16-page table. The range of biostratigraphically important samples is shown on the accompanying diagram. The heavy-mineral concentrates were analyzed by Nancy Stamm; the residues have been returned to Julie Dumoulin. Please note a few (~4 samples have heavy-mineral concentrates that include chalcopyrite and bornite). |
Report by: |
Anita G. Harris
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Referred by: |
Julie A. Dumoulin
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J. H. Dover
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| Age: | Osagean (early middle Osagean) |
Formation: | Kuna Formation |
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Comment: | Age: S. anchoralis-D. latus Zone (early middle Osagean) Biofacies: Scaliognathid; basinal depositional environment. CAI = ~3 11.1 kg or rock processed (320 g 0f +20 mesh and 116 g 20-140 mesh insoluble residue). Heavy-mineral concentrate: chiefly argillaceous grains, and minor iron oxides., barite(?) and micas. |
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