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Macassa Mine

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Book Chapter

Series: Society of Economic Geologists Guidebook Series
Published: 01 January 1991
DOI: 10.5382/GB.11.ch02
EISBN: 9781934969649
.... For a description see paper entitled “Macassa Mine Geology” in this guidebook. ...
Book Chapter

Author(s)
D. F. Cater
Series: Society of Economic Geologists Guidebook Series
Published: 01 January 1991
DOI: 10.5382/GB.11.ch04
EISBN: 9781934969649
... Abstract The Macassa Mine, a division of LAC Minerals Ltd. is situated immediately west of the town of Kirkland Lake, Ontario. It is the only active producer of seven (7) mines located along the famed Mile...
Journal Article
Journal: Economic Geology
Published: 01 August 1984
Economic Geology (1984) 79 (5): 1104–1130.
...R. Kerrich; G. P. Watson Abstract The only remaining gold producer of seven interconnected mines. The district has produced over 710,000 kg Au since 1913. The area is underlain by part of the Timiskaming Group. Three types of gold ore: (1) native Au in chloritic fault gouge or small quartz lenses...
Image
Intramineral phonotephrite dike, stope 4528 MCF, Macassa mine. A. Intramineral dike parallel to the gold-bearing vein exposed in the back of the stope. B. Fragments of vein quartz (highlighted) entirely enclosed within the dike matrix (a cut slab).
Published: 01 September 2008
F ig . 26. Intramineral phonotephrite dike, stope 4528 MCF, Macassa mine. A. Intramineral dike parallel to the gold-bearing vein exposed in the back of the stope. B. Fragments of vein quartz (highlighted) entirely enclosed within the dike matrix (a cut slab).
Book Chapter

Author(s)
D. F. Cater
Series: Society of Economic Geologists Guidebook Series
Published: 01 January 1991
DOI: 10.5382/GB.11.ch01
EISBN: 9781934969649
... gold discovery by Battle Mountain Canada Incorporated) and an introduction to the Macassa Mine geology by D. F. Cater. ...
Series: Society of Economic Geologists Guidebook Series
Published: 01 January 1991
DOI: 10.5382/GB.11.ch09
EISBN: 9781934969649
... Benham on a recent Kirkland Lake gold discovery by Battle Mountain Canada Incorporated) and an introduction to the Macassa Mine geology by D. F. Cater. ...
Book Chapter

Author(s)
D. F. Cater
Series: Society of Economic Geologists Guidebook Series
Published: 01 January 1991
DOI: 10.5382/GB.11.ch10
EISBN: 9781934969649
... Benham on a recent Kirkland Lake gold discovery by Battle Mountain Canada Incorporated) and an introduction to the Macassa Mine geology by D. F. Cater. ...
Series: Society of Economic Geologists Guidebook Series
Published: 01 January 1991
DOI: 10.5382/GB.11
EISBN: 9781934969649
Image
A. Gold-bearing veins associated with the ‘04 Break (stope 4940, Macassa mine), showing a planar white quartz vein, small break-parallel quartz veinlets, and a lens of dark gray quartz. Back and north wall of drift, looking north-northwest. B. Vein along the ‘04 Break, Macassa mine. Note sharp vein contacts, stylolitic surface, slabs, and angular fragments of unfoliated host rock. C. Foliation in the host syenite porphyry along the north contact of the Main Break vein (Discovery outcrop). Looking east. D. Band of breccia consisting of quartz fragments in dark gray cement along the north contact of the Main Break vein at Discovery outcrop. Plan view, looking north. E. Close-up view of a stylolitic band, within a ‘04 Break vein, Macassa mine. F. Polished slab of the Main Break vein, Lake Shore mine, east of shaft 5. The vein contains thin sericitic lenses (src) and inclusions of strongly sericitized wall rocks (wr).
Published: 01 September 2008
F ig . 18. A. Gold-bearing veins associated with the ‘04 Break (stope 4940, Macassa mine), showing a planar white quartz vein, small break-parallel quartz veinlets, and a lens of dark gray quartz. Back and north wall of drift, looking north-northwest. B. Vein along the ‘04 Break, Macassa mine
Image
Examples of shallow- to moderate-dipping hanging-wall viens. A. Vein hosted by mafic syenite and spatially associated with a slip surface (stope 4206-S3, Macassa mine). B. Bedding-parallel vein in tuffs, associated with molybdenite-graphite coated slips. A discordant segment of the vein consists of breccia (wall-rock fragments cemented by quartz). Stope 5030, Macassa mine. C. Remote view of the “E” vein in the proximal hanging wall of the Main Break (Teck-Hughes property, looking west). The vein is hosted by a discrete fault (white arrows).
Published: 01 September 2008
F ig . 20. Examples of shallow- to moderate-dipping hanging-wall viens. A. Vein hosted by mafic syenite and spatially associated with a slip surface (stope 4206-S3, Macassa mine). B. Bedding-parallel vein in tuffs, associated with molybdenite-graphite coated slips. A discordant segment
Image
A. Dark gray, fine-grained quartz filling interstices between randomly oriented coarser prismatic white quartz crystals (vein 4206-S3, Macassa mine). B. Transmitted cross-polarized light photomicrograph of the same vein as in (A); fine-grained quartz in interstices between coarser prismatic quartz crystals. C. Higher magnification photomicrograph of the rectangular area in (B), transmitted plane-polarized light. D. Same view as in (C), reflected plane-polarized light. Note presence of gold (Au), altaite telluride (Te), and opaque nonreflective particles in the dark fine-grained quartz.
Published: 01 September 2008
F ig . 21. A. Dark gray, fine-grained quartz filling interstices between randomly oriented coarser prismatic white quartz crystals (vein 4206-S3, Macassa mine). B. Transmitted cross-polarized light photomicrograph of the same vein as in (A); fine-grained quartz in interstices between coarser
Image
A. Chloritic slip along the Main Break with late (postore) carbonate-quartz veining; back of a drift at the 4500-ft level of the Macassa mine. B, C. Sericitic foliation along the Main Break east of the former Lake Shore shaft 5 (B, plan view facing approximately south; C, cross section view looking west). Foliation (highlighted by dashed lines) is oriented obliquely to fault walls (highlighted by solid lines), which is consistent with oblique reverse-dextral sense of movement. D. Outcrop view of the “Mud Break;” darker bands correspond to sericite-rich foliated domains. E. Close-up cross-sectional view of a foliated sericite-rich band within the “Mud Break.” F. Undeformed symmetrical sericitization halo around a quartz veinlet (“Mud Break” mineralized zone).
Published: 01 September 2008
F ig . 8. A. Chloritic slip along the Main Break with late (postore) carbonate-quartz veining; back of a drift at the 4500-ft level of the Macassa mine. B, C. Sericitic foliation along the Main Break east of the former Lake Shore shaft 5 (B, plan view facing approximately south; C, cross section
Journal Article
Journal: Economic Geology
Published: 01 September 2008
Economic Geology (2008) 103 (6): 1309–1340.
...F ig . 26. Intramineral phonotephrite dike, stope 4528 MCF, Macassa mine. A. Intramineral dike parallel to the gold-bearing vein exposed in the back of the stope. B. Fragments of vein quartz (highlighted) entirely enclosed within the dike matrix (a cut slab). ...
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Journal Article
Published: 01 August 1944
American Mineralogist (1944) 29 (7-8): 299–304.
Image
Estimated δD and δ18O of fluids involved in specified events in the evolution of the southern Superior Province. Reference fields or lines are magmatic water, metamorphic water, ocean water (0W), the meteoric water line (MWL), Alberta and Gulf Coast oilfield brines, and lines for clays at specified temperatures in equilibrium with ambient meteoric water. (A) Archean: 0W, Archean ocean water; involved in regional alteration of volcanic rocks; 1, magmatic water from syntectonic tonalitic granitoid rocks; 2, hydrothermal ore-fluids of lode gold deposits; 3, meteoric water involvement in Eldridge gold deposit, Lac Flavrion pluton, Noranda; citrine-selenite and hematitic overprinting of Larder Lake–Cadillac deformation fault in the Macassa mine, unknown age; 4, fluids for muscovite epidote fractures, Eye-Dashwa lake pluton; 5, magmatic fluids for Pontiac S-type granite Li, Mo, U mineralization; 6, Larder Lake Cadillac deformation zone reactivation at 2510 Ma. (B) Proterozoic and Phanerozoic fluid activity: 7, Paleoproterozoic sedimentary formation brines, locally involved in Ag, Co, -sulpharsenide deposits; 8, adularia vein systems in Eye-Dashwa Lakes granite; 9, hematite chlorite overprinting of 4; 10, brines that alone plot to the left of the MWL from specified mining districts in the Shield; 11, Quaternary glacial waters involved in δD-shifting of Archean serpentines and clays in Quaternary fracture systems; 12, ambient ground waters at Atikokan and the Underground Research Laboratory (URL) that are in isotopic equilibrium with clays of 11.
Published: 02 April 2000
in Eldridge gold deposit, Lac Flavrion pluton, Noranda; citrine-selenite and hematitic overprinting of Larder Lake–Cadillac deformation fault in the Macassa mine, unknown age; 4, fluids for muscovite epidote fractures, Eye-Dashwa lake pluton; 5, magmatic fluids for Pontiac S-type granite Li, Mo, U
Book Chapter

Author(s)
H. L. Lovell
Series: Society of Economic Geologists Guidebook Series
Published: 01 January 1991
DOI: 10.5382/GB.11.ch03
EISBN: 9781934969649
... Abstract The AFTERNOON tour will be by bus, the first 4 stops being in the 10 × 10 km geographic township of Teck, and the 5th is in Lebel, the adjoining Township to the east. From Macassa No.3 shaft return...
Journal Article
Published: 01 May 1940
American Mineralogist (1940) 25 (5): 368–371.
... of the U. S. Geological Survey for the use of the La Plata collection, to Mr. R. D. Hoffman, Mining Geologist, New York City, for the specimens from Cripple Creek, and to the managements of the Lake Shore, Toburn, Wright-Hargreaves, Macassa and Dome mines for the specimens from those properties. The writer...
Journal Article
Journal: Economic Geology
Published: 01 February 2023
Economic Geology (2023) 118 (1): 123–155.
... , The Macassa mine Archean lode gold deposit, Kirkland Lake, Ontario: Geology, patterns of alteration, and hydrothermal regimes : Economic Geology , v. 79 , p. 1104 – 1130 . Kerrich , R. , and Wyman , D. , 1990 , Geodynamic setting of mesothermal gold deposits: An association...
FIGURES | View All (18)
Journal Article
Journal: Economic Geology
Published: 01 June 2024
Economic Geology (2024) 119 (4): 935–965.
..., at the Macassa mine at the Kirkland Lake deposit ( Fig. 1 ), Kerrich and Watson ( 1984 ) showed a proximal increase in K and decrease in Na as a result of the hydrolysis of early albite to muscovite, which may reflect the K-rich nature of the syenitic and alkaline volcanic host rocks to that deposit...
FIGURES | View All (19)
Journal Article
Published: 24 June 2021
The Canadian Mineralogist (2022) 60 (6): 989–1011.
...-tellurides-sulfide mineralization in the Macassa Gold Mine, Abitibi Belt, Canada . Mineralium Deposita 27 66 – 71 . Thompson, J.F.H., Sillitoe, R.H., Baker, T...
FIGURES | View All (11)