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Record #122659:

Glacial history, drift composition, and mineral exploration, central Labrador / R.A. Klassen, F.J. Thompson.

Title: Glacial history, drift composition, and mineral exploration, central Labrador / R.A. Klassen, F.J. Thompson.
Author(s): Klassen, R. A.
Thompson, F. J.
Date: 1993.
In: Geological Survey of Canada. Bulletin. (1993.), Vol. 435 (1993)
Abstract: Ice-flow history and drift composition were investigated between 1984 and 1988 to establish geological framework for mineral exploration. Striae indicate complex history of ice flow, indicating marked change in ice flow direction not shown by glacially streamlined landforms. Shape and orientation of glacial dispersal trains record erosion and transport during succeeding ice-flow events. Regional till composition reflects compositional differences between major geological units and terrains. Glacial dispersal trains can mask bedrock tens to hundreds of kilometres down-ice and can be recognized on geochemical and lithological maps.
Notes:

Geological Survey of Canada. Bulletin. Vol. 435 :v, 1-76 (1993).

In slip case.

Keywords: 551.33 -- Glacial geology.
551.332.212 -- Till or boulder clay.
551.331.55 -- Rock, polished, grooved and striated by glacial action.
551.336 -- Ice ages.
551.79 -- Quaternary.
553 -- Economic geology.
54 -- Chemistry.
553.061.16 -- Diagenesis, ore deposits.
550.4 -- Geochemistry.
622 -- Mining.
622.1 -- Mineral deposits, preliminary investigations.
E7 -- Glaciology: glacial geology and ice ages.
(*41) -- Canada.
(*423) -- Labrador.
SPRI record no.: 122659

MARCXML

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100 1# ‡aKlassen, R. A.
245 10 ‡aGlacial history, drift composition, and mineral exploration, central Labrador /‡cR.A. Klassen, F.J. Thompson.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1993.
300 ## ‡ap. v, 1-76 :‡bill., diags., tables, maps +‡efolded sheet of maps.
500 ## ‡aGeological Survey of Canada. Bulletin. Vol. 435 :v, 1-76 (1993).
500 ## ‡aIn slip case.
520 3# ‡aIce-flow history and drift composition were investigated between 1984 and 1988 to establish geological framework for mineral exploration. Striae indicate complex history of ice flow, indicating marked change in ice flow direction not shown by glacially streamlined landforms. Shape and orientation of glacial dispersal trains record erosion and transport during succeeding ice-flow events. Regional till composition reflects compositional differences between major geological units and terrains. Glacial dispersal trains can mask bedrock tens to hundreds of kilometres down-ice and can be recognized on geochemical and lithological maps.
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.332.212 -- Till or boulder clay.‡2udc
650 07 ‡a551.331.55 -- Rock, polished, grooved and striated by glacial action.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡a553 -- Economic geology.‡2udc
650 07 ‡a54 -- Chemistry.‡2udc
650 07 ‡a553.061.16 -- Diagenesis, ore deposits.‡2udc
650 07 ‡a550.4 -- Geochemistry.‡2udc
650 07 ‡a622 -- Mining.‡2udc
650 07 ‡a622.1 -- Mineral deposits, preliminary investigations.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*41) -- Canada.‡2udc
651 #7 ‡a(*423) -- Labrador.‡2udc
700 1# ‡aThompson, F. J.
773 0# ‡7nnas ‡tGeological Survey of Canada. Bulletin. ‡gVol. 435 (1993) ‡wSPRI-19826
917 ## ‡aUnenhanced record from Muscat, imported 2019
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