Sample: |
Sample No. 91Tr47B -- USGS No. 31848-PC
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Locality: |
Field No. 91Tr47B
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Description: |
Howard Pass C-3. North-south traverse through section of unit Mlb: 68o 30.6' N., 157o 32.45' W. (base, 47A) to 68o 30.5' N., 157o 32.45' W. (top, 47F). Sample from <5 m-thick interval of thick-bedded, dark-gray to brownish-gray, fine-grained, encrinitic limestone. Thin section is skeletal grainstone; bioclasts mostly bryozoans and lesser crinoid ossicle and brachiopods. Some bioclasts partly silicified; others have micritized rims. Local areas of dolomitic mud rich in calcareous spicules; some muddy zones may be burrows. Heavy-mineral concentrate includes phosphatic brachiopod fragments. (description from Dover et al., 2004, p. 39 (Table 1)); [Howard Pass C-3 quad. 68°30.60', 157°32.45'. Lisburne Group (Brooks Range allochthon); <5 m interval of thick-bedded, dark-gray to brownish-gray, fine-grained, encrinitic limestone. Thin section is skeletal grainstone. Skeletals mostly bryozoans, lesser crinoid ossicles and brachiopods. Some skeletals partly silicified; others have micritized rims. Local areas of dolomitic mud rich in calcareous spicules; some muddy zones may be burrows. (description from Harris E&R report dated Sept. 17, 1993; Shipment no. A-93-11)] |
Location: |
Alaska Quadrangle: Howard Pass C-3 Lat.: 68o30.6 ' Long.: 157o32.45 ' |
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Reference
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Title: |
Report on Referred Fossils
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1993
(09/17)
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This report is long (1.5 years) overdue, but I have been exceedingly busy writing papers, responding to reviewers and editors comments and preparing talks. I am finally returning to a partial E&R mode and your collections were at the top of the list. |
Report by: |
Anita G. Harris
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Referred by: |
Irv L. Tailleur
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John S. Kelley
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| Age: | Kinderhookian-Osagean (late Kinderhookian - early Osagean) |
Formation: | Lisburne Group |
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Comment: | Age: late Kinderhookian-early Osagean Biofacies: Indeterminate Thin section description by Julie A. Dumoulin. CAI = 1.5-2 Heavy-mineral concentrate: chiefly iron-oxide or weathered pyrite steinkerns and iron oxides and minor amounts of dolomite and phosphatic brachiopod fragments. |
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