Volcanic Reconstruction of the Archean North Rhyolite, Kidd Creek Mine, Timmins, Ontario, Canada
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January 2004 Issue 80 Volcanic Reconstruction of the Archean North Rhyolite, Kidd Creek Mine, Timmins, Ontario, Canada Michelle DeWolfe Harold L. Gibson Mineral Exploration Research Centre Laurentian University Ramsey Lake Road, Sudbury, Ontario, P3E 6B5, Email: [email protected] David Richardson Falconbridge Limited Kidd Mining Division, PO Box 2002, Hwy 655, Timmins, Ontario, P4N 7K1 John Ayer Ontario Geological Survey Willet Green Miller Centre, Ramsey Lake Road, Sudbury, Ontario, P3E 6B5 Fig. 1. General geology map showing the Abitibi greenstone belt and Introduction the location of the Kidd Creek mine approximately 24 km north of A succession of volcanic rocks collectively known as the Timmins (modified from Bleeker and Hester, 1999). North Rhyolite (NR) is located directly northeast of the giant Kidd Creek Cu-Zn-Ag volcanogenic massive sulfide (VMS) thermal alteration away from the deposit. Understanding the deposit, within the Abitibi greenstone belt of the Superior prov- large-scale volcanic environment, which hosts the NR and the ince (Figs. 1 and 2). The NR has been interpreted as a lateral Kidd Creek orebodies, will allow a better comparison between extension of the Kidd Creek mine stratigraphy (Hannington et the environment in which the Kidd Creek deposit formed and the al., 1999a). However, detailed work on the stratigraphy and environment of formation for other VMS deposits. This may structure of the NR, and its relationship to the mine stratigraphy, also help to create a better understanding of the environments is not available in existing literature. and processes that favor the generation of giant VMS deposits. It The objectives of this study are to 1) establish the structural is also anticipated that an understanding of the volcanic environ- and stratigraphic relationship between the NR and the Kidd ment, and knowledge of the distribution of volcanic rocks and Creek mine rhyolite, and 2) reconstruct the volcanic environ- hydrothermal alteration, will aid in the exploration for new VMS ment of the NR, post-rhyolite volcanism to better constrain the deposits in the Kidd Creek area. volcanic setting and environment of the Kidd Creek massive sulfide deposit. Geological Setting and Stratigraphy of the North Rhyolite In this study, a The NR has been interpreted to represent a lateral extension Inside this issue: reconstruction of of the Kidd Creek mine stratigraphy. A U-Pb zircon age of the NR is used, 2716.0 ± 0.5 Ma for the massive aphyric rhyolite of the NR, Letter from the Editor 3 for the first time, similar to the U-Pb zircon age of 2716.0± 0.6 Ma for the massive to constrain the Timmins Field Conference 10 aphyric rhyolite of the Kidd Creek mine stratigraphy supports large-scale vol- this interpretation (Bleeker et al., 1999). Bleeker (1999) pro- Book Review 12 canic environment, posed that faults that slice through the Kidd Creek mine fold, which hosts the CIM AGM Edmonton 16 and display a net sinistral movement, have displaced the north- Kidd Creek de- ern limb of the Kidd Creek mine fold up to 2 km to the north- posit and to assess Calendar of Events 18 (Continued on page 4) the scale of hydro- 2003-2004 MINERAL DEPOSITS DIVISION EXECUTIVE LIST MDD Goals and Objectives Chairperson: Moira Smith The Gangue is published quarterly by the Min- TECK COMINCO Limited, #600 - 200 Burrard Street eral Deposits Division of GAC and is distrib- Vancouver, BC V6C 3L9; Tel: (604) 640-5373; Fax: (604) 685-3069 uted to its members. 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