14,651 research outputs found
Letter from Thomas C. Linn to John Sloan, October 4, 1939
No full text1 leaf (double-sided)Letter from Thomas C. Linn to John Sloan, October 4, 193
Letter from Thomas C. Linn to John Sloan, October 4, 1939
No full text1 leaf (double-sided)Letter from Thomas C. Linn to John Sloan, October 4, 193
Linn county barn context
No full textMary K. Gallagher, with assisstance provided by Joni Nelson, May Dasch, Pat Dunn, Beth Fox, Philip Dole, project consultant.Title from PDF title page (viewed on January 28, 2020).This archived document is maintained by the State Library of Oregon as part of the Oregon Documents Depository Program. It is for informational purposes and may not be suitable for legal purposes.Includes bibliographical references.Financed in part with Federal funds from the National Park Service, U.S. Dept. of the Interior, as provided by the State Historic Preservation Office.Mode of access: Internet from the Oregon Government Publications Collection.Text in English
Data for: The Relation Between Petroleum Product Futures Prices and Crude Oil Futures Prices
No full textData used in the study: The Relation Between Petroleum Product Futures Prices and Crude Oil Futures Prices Authors: Louis H. Ederington*, Chitru S. Fernando*, Thomas K. Lee**, Scott C. Linn**Price College of BusinessUniversity of Oklahoma307 West Brooks, Norman, OK 73019**U.S. Energy Information Administration, U.S. Department of Energy1000 Independence Ave., SW Washington, DC 2058
Linn - Thomas C. Linn
No full textA.B.; A.M, 1883; Sigma Chi; Phrenakosmian; editor, College Monthly, 1880-1; orator, anniversary, 1880; entered Freshman, 1877. Born Jan. 26, 1860. Rowan County, N.C. Parents, Robert J. and Joicy C. Practicing Law, Salisbury, N.C., 1884- . Mayor of Salisbury, N.C., 1886-1902 and 1906-08; supt. of instruction, Rowan County, N.C., 1883-86. Died April 18, 1932. Married Oct. 22, 1884, Annie D. Stahle, Gettysburg, who died July 5, 1926. Children, Stahle; Mary K.; Thomas C. Address: Salisbury, N.C. Handwritten on back: ""T. C. Linn, Salisbury, N.C., class '81"
Morphometrics confirm taxonomic deflation in dwarf lemurs (Primates: Cheirogaleidae), as suggested by genetics
No full textFigure 2. Allometric and non-allometric craniodental characters in Cheirogaleus. (A) Palatal length (PALL), (B) temporal line (TpLi), and (C) second premolar height (P2), given in mm, are scaled against the greatest skull length (GSKL) for Cheirogaleus medius, Cheirogaleus adipicaudatus, Cheirogaleus major, Cheirogaleus ravus, Cheirogaleus sibreei, and unknown specimens, as assessed by Groves (2000).Published as part of Groeneveld, Linn F., Rasoloarison, Rodin M. & Kappeler, Peter M., 2011, Morphometrics confirm taxonomic deflation in dwarf lemurs (Primates: Cheirogaleidae), as suggested by genetics, pp. 229-244 in Zoological Journal of the Linnean Society 161 (1) on page 235, DOI: 10.1111/j.1096-3642.2010.00634.x, http://zenodo.org/record/575625
Matthew Passion BWV 244 : Bach's last performing version, c. 1742
No full textPublisher no.: Linn CKD 313
High resolution carbon isotope stratigraphy of the basal Silurian stratotype (Dob's Linn, Scotland) and its global correlation
No full textSince its designation as the Global Stratotype Section and Point (GSSP) for the base of the Silurian System, the choice of Dob's Linn, Southern Scotland, has received criticism due to the difficulties of relating its well constrained graptolite biostratigraphy to shallow water sequences elsewhere. Kerogen samples from across the Ordovician-Silurian boundary interval at Dob's Linn have yielded carbon stable isotope signatures consistent with those recorded elsewhere, in particular showing a clear positive δ13C excursion in the terminal Ordovician. The architecture of the δ13C curve from Dob's Linn enables very high resolution stratigraphic subdivision and direct correlation between the deep water Dob's Linn section and time equivalent carbonate shelf deposits. An integrated stratigraphic scheme using isotope stratigraphy and biostratigraphy of graptolites, conodonts and shelly faunas has been constructed. This direct correlation shows that the shallow water successions, including the former stratotype candidate at Anticosti Island, are generally incomplete, with hiatuses related to the rapid sea level changes during the Hirnantian stage. This confirms and greatly increases the global utility of Dob's Linn as a boundary stratotype
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