Late Paleozoic magnetization of mineralized and unmineralized ordovician carbonates from east Tennessee: Evidence for a post‐ore chemical event
- 10 December 1987
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 92 (B13) , 14165-14176
- https://doi.org/10.1029/jb092ib13p14165
Abstract
No abstract availableKeywords
This publication has 30 references indexed in Scilit:
- Thermally activated viscous remanence in some magnetite‐ and hematite‐bearing dolomitesGeophysical Research Letters, 1986
- Thermoviscous remagnetization in some Appalachian limestonesGeophysical Research Letters, 1985
- Deposition and dolomitization of Upper Knox carbonate sediments, Copper Ridge district, East TennesseeGSA Bulletin, 1982
- A Least-Squares Method to find a Remanence Direction from Converging Remagnetization CirclesGeophysical Journal International, 1976
- Paleomagnetism and the Origin of Mississippi Valley-Type Ore DepositsCanadian Journal of Earth Sciences, 1974
- Appalachian strata-bound deposits; their essential features, genesis and the exploration problemEconomic Geology, 1971
- A lower Paleozoic paleoaquifer; the Kingsport Formation and Mascot dolomite of Tennessee and southwest VirginiaEconomic Geology, 1971
- Genesis of the Ordovician zinc deposits in east TennesseeEconomic Geology, 1965
- Ore deposits and sedimentary features, Jefferson City Mine, TennesseeEconomic Geology, 1960
- Dispersion on a SphereProceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, 1953