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Record #177070:

Geology of the Miramar Con mine / R.L. Hauser, D.W. McDonald, J.P. Siddorn.

Title: Geology of the Miramar Con mine / R.L. Hauser, D.W. McDonald, J.P. Siddorn.
Author(s): Hauser, R. L.
McDonald, D. W.
Siddorn, J. P.
Date: 2006.
Publisher: St John's, Nfld: Geological Association of Canada, Mineral Deposits Division
In: Gold in the Yellowknife Greenstone Belt, Northwest Territories : results of the EXTECH III multidisciplinary research project. (2006.),
Abstract: Reports that gold at Miramar Con mine, on west shore of Yellowknife Bay, is hosted in two large, continuous parallel shear zones and several peripheral narrower shears and quartz-vein systems. Ore within shears occurs within quartz lenses forming numerous steeply plunging ore trends and few large ovoid trends. Subparallel steeply plunging trends indicate possibility of original structural control to ore deposition.
Notes:

In: Gold in the Yellowknife Greenstone Belt, Northwest Territories : results of the EXTECH III multidisciplinary research project / C.D. Anglin, H. Falck, D.F. Wright, E.J. Ambrose, eds.

Keywords: 551.1/.4 -- Geology.
551.7 -- Stratigraphy.
553 -- Economic geology.
553.042 -- Mineral resources.
553.411 -- Gold deposits, minerals.
622 -- Mining.
622.342.1 -- Gold mining.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*41) -- Canada.
(*440) -- Northwest Territories.
SPRI record no.: 177070

MARCXML

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001 SPRI-177070
005 20220930074802.0
007 ta
008 220930s2006####nfcab##|#####|0||#0#eng#d
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040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aHauser, R. L.
245 10 ‡aGeology of the Miramar Con mine /‡cR.L. Hauser, D.W. McDonald, J.P. Siddorn.
260 ## ‡aSt John's, Nfld :‡bGeological Association of Canada, Mineral Deposits Division,‡c2006.
300 ## ‡ap. 173-187 :‡bill., diags., table, maps.
500 ## ‡aIn: Gold in the Yellowknife Greenstone Belt, Northwest Territories : results of the EXTECH III multidisciplinary research project / C.D. Anglin, H. Falck, D.F. Wright, E.J. Ambrose, eds.
520 3# ‡aReports that gold at Miramar Con mine, on west shore of Yellowknife Bay, is hosted in two large, continuous parallel shear zones and several peripheral narrower shears and quartz-vein systems. Ore within shears occurs within quartz lenses forming numerous steeply plunging ore trends and few large ovoid trends. Subparallel steeply plunging trends indicate possibility of original structural control to ore deposition.
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a551.7 -- Stratigraphy.‡2udc
650 07 ‡a553 -- Economic geology.‡2udc
650 07 ‡a553.042 -- Mineral resources.‡2udc
650 07 ‡a553.411 -- Gold deposits, minerals.‡2udc
650 07 ‡a622 -- Mining.‡2udc
650 07 ‡a622.342.1 -- Gold mining.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*41) -- Canada.‡2udc
651 #7 ‡a(*440) -- Northwest Territories.‡2udc
700 1# ‡aMcDonald, D. W.
700 1# ‡aSiddorn, J. P.
773 0# ‡7nnam ‡aC.D. Anglin, H. Falck, D.F. Wright, E.J. Ambrose, eds. ‡tGold in the Yellowknife Greenstone Belt, Northwest Territories : results of the EXTECH III multidisciplinary research project. ‡dSt John's, Nfld : Geological Association of Canada, Mineral Deposits Division, 2006. ‡wSPRI-176792
916 ## ‡aJW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220930 ‡bJW