Geologic Map of the Line Point Quadrangle, Boundary County Idaho, and Lincoln County, Montana
IDAHO GEOLOGICAL SURVEY IDAHOGEOLOGY.ORG IGS DIGITAL WEB MAP 150 MONTANA BUREAU OF MINES AND GEOLOGY MBMG.MTECH.EDU MBMG OPEN FILE 623 white graded or nongraded argillite tops. Conspicuous bar code-like REFERENCES patterns in the middle, formed by alternating dark and light siltite, persist regionally (Huebschman, 1973) and have been used as markers for correla- GEOLOGIC MAP OF THE LINE POINT QUADRANGLE, BOUNDARY COUNTY, IDAHO, AND tion by Cominco (Hamilton and others, 2000). Siltite and argillite couplets, Anderson, H.E., and D.W. Davis, 1995, U-Pb geochronology of the Moyie sills, with dark, less commonly light tops, have even and parallel, uneven, wavy Purcell Supergroup, southeastern British Columbia: Implications for the or undulating lamination. Rusty nature of outcrop is due to weathering of Mesoproterozoic geological history of the Purcell (Belt) basin: Canadian CORRELATION OF MAP UNITS abundant sulfides, commonly pyrrhotite. Dominant lamination style and Journal of Earth Sciences, v. 32, no. 8, p. 1180-1193. LINCOLN COUNTY, MONTANA concentration of sulfides vary between members. Quartzite in 2-20 dm beds Anderson, H.E., and W.D. Goodfellow, 2000, Geochemistry and isotope chem- Alluvial and Colluvium and Glacial and Related Deposits is light weathering, averages about 60 percent quartz, 20 percent plagio- istry of the Moyie sills: Implications for the early tectonic setting of the Lacustrine Deposits Mass Wasting Deposits clase, with the rest mostly white micas and 5 percent biotite (Cressman, Mesoproterozoic Purcell basin, in J.W. Lydon, Trygve Höy, J.F. Slack, and 1989). Previous mapping in this area and to the east by Cressman and Harri- M.E.
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