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pure and applied geophysics (297)
Bibliography

Wallace, R. E., & Morris, H. T. (1986). Characteristics of faults and shear zones in deep mines. Pure and Applied Geophysics, 124(1–2), 107–125.

Authors 2
  1. Robert E. Wallace (first)
  2. Hal T. Morris (additional)
References 10 Referenced 94
  1. Charlewood, G. H. (1964),Geology of deep developments of the main ore zone at Kirkland Lake: Compilation. Ontario Dept. Mines Geol.,Circular 11, 49 pp.
  2. Fryklund, V. C., Jr. (1964),Ore deposits of the Coeur d'Alene district, Shoshone Country, Idaho. U.S. Geol. Surv. Prof. Paper 445, 103 pp. (10.3133/pp445)
  3. Hobbs, S. W., Griggs, A. B., Wallace, R. E. andCampbell, A. B. (1965),Geology of the Coeur d'Alene district, Shoshone County, Idaho. U.S. Geol. Surv. Prof. Paper 478, 139 pp. (10.3133/pp478)
  4. Hopkins, H. (1950),Geology of the Wright-Hargreaves mine. Ontario Dept. Mines Ann. Rept., 1948,57, Pt. 5, pp. 161–176. / Ontario Dept. Mines Ann. Rept. by H. Hopkins (1950)
  5. Mills, J. W. (1950),Structural control of ore bodies as illustrated by the use of vein contours at the O'Brien gold mine, Cadillac, Quebec. Econ. Geol.45, 786–807. (10.2113/gsecongeo.45.8.786) / Econ. Geol. by J. W. Mills (1950)
  6. Morris, H. T. (1968), ‘The main Tintic mining district, Utah’, inOre Deposits of the United States, 1933–1967. Am. Inst. Min. Met. Pet. Engrs., II, pp. 1043–1073.
  7. Morris, H. T. andLovering, T. S. (1979),General geology and mines of the East Tintic mining district, Utah and Juab Counties, Utah. U.S. Geol. Surv. Prof. Paper 1024, 203 pp.
  8. Ransome, F. L. andCalkins, F. C. (1908),Geology and ore deposits of the Coeur d'Alene district, Idaho. U.S. Geol. Surv. Prof. Paper 62, 203 pp. (10.3133/pp62)
  9. Wallace, R. E., Griggs, A. B. Campbell, A. B. andHobbs, S. W. (1960), ‘Tectonic settings of the Coeur d'Alene district, Idaho’, inShort Papers in the Geological Sciences. U.S. Geol. Surv. Prof. Paper 400-B, pp. B25–B27.
  10. Wallace, R. E. andMorris, H. T. (1979), ‘Characteristics of faults and shear zones as seen in mines at depths as much as 2.5 km below the surface’, inProc. Conf. VIII, Analysis of Actual Fault Zones in Bedrock J. Evernden (ed.). U.S. Geol. Surv. Open-File Rept. 79-1239, p. 79–100.
Dates
Type When
Created 20 years, 8 months ago (Dec. 24, 2004, 3:10 p.m.)
Deposited 1 year, 1 month ago (July 26, 2024, 3:28 a.m.)
Indexed 2 weeks, 4 days ago (Aug. 19, 2025, 6:36 a.m.)
Issued 39 years, 8 months ago (Jan. 1, 1986)
Published 39 years, 8 months ago (Jan. 1, 1986)
Published Print 39 years, 8 months ago (Jan. 1, 1986)
Funders 0

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@article{Wallace_1986, title={Characteristics of faults and shear zones in deep mines}, volume={124}, ISSN={1420-9136}, url={http://dx.doi.org/10.1007/bf00875721}, DOI={10.1007/bf00875721}, number={1–2}, journal={pure and applied geophysics}, publisher={Springer Science and Business Media LLC}, author={Wallace, Robert E. and Morris, Hal T.}, year={1986}, month=jan, pages={107–125} }