Superior Craton Geological
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Northwestern Superior Craton Margin, Manitoba: an Overview of Archean
GS-7 Northwestern Superior craton margin, Manitoba: an overview of Archean and Proterozoic episodes of crustal growth, erosion and orogenesis (parts of NTS 54D and 64A) by R.P. Hartlaub1, C.O. Böhm, L.M. Heaman2, and A. Simonetti2 Hartlaub, R.P., Böhm, C.O., Heaman, L.M. and Simonetti, A. 2005: Northwestern Superior craton margin, Manitoba: an overview of Archean and Proterozoic episodes of crustal growth, erosion, and orogenesis (parts of NTS 54D and 64A); in Report of Activities 2005, Manitoba Industry, Economic Development and Mines, Manitoba Geological Survey, p. 54–60. Summary xenocrystic zircon, and in the The northwestern margin of the Superior Province in isotopic signature of Neoarchean Manitoba represents a dynamic boundary zone with good granite bodies (Böhm et al., 2000; potential for magmatic, sedimentary-hosted, and structur- Hartlaub et al., in press). The ALCC extends along the ally controlled mineral deposits. The region has a history Superior margin for at least 50 km, and may have a com- that commences in the early Archean with the formation mon history with other early Archean crustal fragments of the Assean Lake Crustal Complex. This fragment of in northern Quebec and Greenland (Hartlaub et al., in early to middle Archean crust was likely accreted to the press). Superior Province between 2.7 and 2.6 Ga, a major period South of the ALCC, the Split Lake Block repre- of Superior Province amalgamation. Sediments derived sents a variably retrogressed and shear zone–bounded from this amalgamation process were deposited at granulite terrain that is dominated by plutonic rocks and numerous locations along the northwestern margin of mafic granulite (Hartlaub et al., 2003, 2004). -
The Penokean Orogeny in the Lake Superior Region Klaus J
Precambrian Research 157 (2007) 4–25 The Penokean orogeny in the Lake Superior region Klaus J. Schulz ∗, William F. Cannon U.S. Geological Survey, 954 National Center, Reston, VA 20192, USA Received 16 March 2006; received in revised form 1 September 2006; accepted 5 February 2007 Abstract The Penokean orogeny began at about 1880 Ma when an oceanic arc, now the Pembine–Wausau terrane, collided with the southern margin of the Archean Superior craton marking the end of a period of south-directed subduction. The docking of the buoyant craton to the arc resulted in a subduction jump to the south and development of back-arc extension both in the initial arc and adjacent craton margin to the north. A belt of volcanogenic massive sulfide deposits formed in the extending back-arc rift within the arc. Synchronous extension and subsidence of the Superior craton resulted in a broad shallow sea characterized by volcanic grabens (Menominee Group in northern Michigan). The classic Lake Superior banded iron-formations, including those in the Marquette, Gogebic, Mesabi and Gunflint Iron Ranges, formed in that sea. The newly established subduction zone caused continued arc volcanism until about 1850 Ma when a fragment of Archean crust, now the basement of the Marshfield terrane, arrived at the subduction zone. The convergence of Archean blocks of the Superior and Marshfield cratons resulted in the major contractional phase of the Penokean orogeny. Rocks of the Pembine–Wausau arc were thrust northward onto the Superior craton causing subsidence of a foreland basin in which sedimentation began at about 1850 Ma in the south (Baraga Group rocks) and 1835 Ma in the north (Rove and Virginia Formations). -
Uranium Deposits of Ontario- Their Distribution and Classification
Ontario Geological Survey Miscellaneous Paper 86 The Uranium Deposits of Ontario- Their Distribution and Classification By James A. Robertson 1981 lanWPope Ministry of !^st£ Natural ...__ W.T. Foster Deputy Minister Ontario ®OMNR-OGS 1981 ISSN 0704-2752 Printed in Canada ISBN 0-7743-602627 Publications of the Ontario Ministry of Natural Resources and price list are available through the Ministry of Natural Resources, Public Service Centre Room 1640, Whitney Block, Queen's Park, Toronto, Ontario, M7A 1W3 (personal shopping and mail orders). and reports only from the Ontario Government Bookstore, Main Floor 880 Bay St., Toronto for per- sonal shopping. Out-of-Town customers write to Ministry of Government Services, Publica- tions Services Section, 5th Floor, 880 Bay St., Toronto. Ontario. M7A 1N8. Telephone 965-6015. Toll free long distance 1 •800-268-7540, in Area Code 807 dial 0-Zenith 67200. Orders for publications should be accompanied by cheque or money order payable to the Treasurer of Ontario. Every possible effort is made to ensure the accuracy of the information con- tained in this report, but the Ministry of Natural Resources does not assume any liability for errors that may occur. Source references are included in the report and users may wish to verify critical information. Parts of this publication may be quoted if credit is given. It is recommended that reference to this report be made in the following form: Robertson, James A. 1981: The Uranium Deposits ol Ontario-Their Distribution and Classifica- tion; Ontario Geological -
Lithospheric Architecture Beneath Hudson Bay 10.1002/2015GC005845 Robert W
PUBLICATIONS Geochemistry, Geophysics, Geosystems RESEARCH ARTICLE Lithospheric architecture beneath Hudson Bay 10.1002/2015GC005845 Robert W. Porritt1, Meghan S. Miller1, and Fiona A. Darbyshire2 Special Section: 1 2 The Lithosphere- Department of Earth Sciences, University of Southern California, Los Angeles, California, USA, Centre de recherche asthenosphere System GEOTOP, UniversiteduQu ebec a Montreal, Montreal, Quebec, Canada Key Points: Abstract Hudson Bay overlies some of the thickest Precambrian lithosphere on Earth, whose internal The thick lithosphere of Hudson Bay has significant structural variation structures contain important clues to the earliest workings of plate formation. The terminal collision, the We directly image the thermal Trans-Hudson Orogen, brought together the Western Churchill craton to the northwest and the Superior blanketing on the asthenosphere craton to the southeast. These two Archean cratons along with the Paleo-Proterozoic Trans-Hudson inter- The lithospheric thickness of Hudson Bay is 200–350 km nides, form the core of the North American craton. We use S to P converted wave imaging and absolute shear velocity information from a joint inversion of P to S receiver functions, new ambient noise derived Supporting Information: phase velocities, and teleseismic phase velocities to investigate this region and determine both the thick- Supporting Information S1 ness of the lithosphere and the presence of internal discontinuities. The lithosphere under central Hudson Software S1 Bay approaches 350 km thick but is thinner (200–250 km) around the periphery of the Bay. Furthermore, the amplitude of the LAB conversion from the S receiver functions is unusually large for a craton, suggesting Correspondence to: a large thermal contrast across the LAB, which we interpret as direct evidence of the thermal insulation R. -
Great Lakes Tectonic Zone in Marquette Area, Michigan Implications for Archean Tectonics in North-Central United States
Great Lakes Tectonic Zone in Marquette Area, Michigan Implications for Archean Tectonics in North-Central United States U.S. GEOLOGICAL SURVEY BULLETIN 1904-E AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the cur rent-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Sur vey publications released prior to the current year are listed in the most recent annual "Price and Availability List." Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated month ly, which is for sale in microfiche from the U.S. Geological Survey, Books and Open-File Reports Section, Federal Center, Box 25425, Denver, CO 80225. Reports released through the NTIS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Techniques of Water-Resources Investigations, Circulars, publications of general in Books -
Isotopic Mapping of the Continental Crust: a New Area Selection Tool David Mole, Laurentian University, Sudbury, Canada the Area
Isotopic mapping of the continental crust: A new area selection tool David Mole, Laurentian University, Sudbury, Canada The area selection process is a critical component of exploration targeting. It requires incremental down-scaling, from the planetary-scale, through continent, terrane, and regional scales, using predictive methods, to the belt-scale, where detective methods can be used. Despite the constant search for new tools and technology, the value of new discoveries is currently less than the exploration investment, across a wide range of commodities. This is unsustainable, and demonstrates an urgent need to: (1) push into new search spaces which may be deep, covered, or remote; and (2) develop more effective multi-scale exploration tools for use in these new spaces. Over last 10-15 years, the large-scale spatial application of isotopic data has been shown to effectively image the cryptic architecture of continental areas. Lithospheric and crustal architecture – the framework of major tectonic blocks, terranes and their boundaries – represents a fundamental first-order control on ore deposits and the location of world-class mineral camps. Focused mainly (but not exclusively) within Archean cratons, researchers have constrained the time-resolved lithospheric architecture of large swathes of the continental crust. Champion and Cassidy (2007) used regional Sm-Nd isotopic data to map the crustal architecture of the Yilgarn Craton (Western Australia), and Mole et al. (2013) demonstrated the association between that lithospheric architecture and BIF-hosted iron, orogenic gold, and komatiite-hosted Ni-Cu-PGE systems. Those results demonstrated the underlying control of lithospheric architecture and the potential for isotopic mapping as a greenfields area-selection tool. -
Geology of the Grand River Watershed an Overview of Bedrock and Quaternary Geological Interpretations in the Grand River Watershed
Geology of the Grand River Watershed An Overview of Bedrock and Quaternary Geological Interpretations in the Grand River watershed Prepared by Bob Janzen, GIT December 2018 i Table of Contents List of Maps ..................................................................................................................... iii List of Figures .................................................................................................................. iii 1.0 Introduction ........................................................................................................... 1 2.0 Bedrock Geology .................................................................................................. 1 Algonquin Arch ......................................................................................................... 2 Bedrock Cuestas ...................................................................................................... 3 2.1 Bedrock Surface ................................................................................................. 4 2.2 Bedrock Formations of the Grand River watershed ........................................... 8 2.2.1 Queenston Formation ................................................................................ 15 2.2.2 Clinton–Cataract Group ............................................................................. 15 2.2.2.1 Whirlpool Formation ............................................................................ 16 2.2.2.2 Manitoulin Formation .......................................................................... -
Geology Datasets of North America for Use with Ice Sheet Models Evan J
Discussions Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2018-139 Earth System Manuscript under review for journal Earth Syst. Sci. Data Science Discussion started: 22 November 2018 c Author(s) 2018. CC BY 4.0 License. Open Access Open Data Geology datasets of North America for use with ice sheet models Evan J. Gowan1, Lu Niu1, Gregor Knorr1, and Gerrit Lohmann1 1Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany Correspondence: Evan J. Gowan ([email protected]) Abstract. The ice-substrate interface is an important boundary condition for ice sheet modelling. The substrate affects the ice sheet by allowing sliding through sediment deformation and accommodating the storage and drainage of subglacial water. We present three datasets with different geological parameters for the region that was covered by the ice sheets in North America, including 5 Greenland and Iceland. The first dataset includes the distribution surficial sediments, which is separated into continuous, discontinuous and predominantly rock categories. The second dataset includes sediment grain size properties, which is divided into three classes: clay, silt and sand, based on the dominant grain size of the glacial sediments. The third dataset is the generalized bedrock geology. We demonstrate the utility of these datasets for governing ice sheet dynamics by using an ice sheet model with a simulation that extends through the last glacial cycle. Changes in ice thickness by up to 40% relative to 10 a reference simulation happened when the shear friction angle was reduced to account for a weaker substrate. These datasets provide a basis to improve the basal boundary conditions in ice sheet models. -
Seamless Quaternary Geology of Southern Ontario
Miscellaneous Release—Data 128 – Revised Surficial Geology of Southern Ontario Project Summary and Technical Document Originally released as MRD 128 in October 2003 Revised version of MRD 128 (MRD 128—Revised) released April 2010 Table of Contents ABSTRACT ...................................................................................................................................................3 INTRODUCTION...........................................................................................................................................4 GENERAL QUATERNARY GEOLOGY OF SOUTHERN ONTARIO...........................................................4 DATA SOURCES..........................................................................................................................................5 QUATERNARY/SURFICIAL GEOLOGY MAPS......................................................................................................5 OTHER DATA SOURCES ............................................................................................................................6 FIELD INVESTIGATIONS .................................................................................................................................6 BEDROCK GEOLOGY MAPS............................................................................................................................6 AERIAL PHOTO INTERPRETATION...................................................................................................................6 AGGREGATE RESOURCES -
Constraining the Formation and Alteration of Sudbury Breccia, Ontario, Canada: Implications for Footwall Cu-Ni-PGE Exploration
Western University Scholarship@Western Electronic Thesis and Dissertation Repository 9-6-2016 12:00 AM Constraining the Formation and Alteration of Sudbury Breccia, Ontario, Canada: Implications for Footwall Cu-Ni-PGE Exploration Jonathan W. O'Callaghan The University of Western Ontario Supervisor Dr. G.R. Osinski The University of Western Ontario Joint Supervisor Dr. R.L. Linnen The University of Western Ontario Graduate Program in Geology A thesis submitted in partial fulfillment of the equirr ements for the degree in Master of Science © Jonathan W. O'Callaghan 2016 Follow this and additional works at: https://ir.lib.uwo.ca/etd Part of the Geology Commons Recommended Citation O'Callaghan, Jonathan W., "Constraining the Formation and Alteration of Sudbury Breccia, Ontario, Canada: Implications for Footwall Cu-Ni-PGE Exploration" (2016). Electronic Thesis and Dissertation Repository. 4075. https://ir.lib.uwo.ca/etd/4075 This Dissertation/Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. i Abstract Sudbury breccia is an impactite situated in the footwall of the 1.85 Ga Sudbury impact structure, situated in Ontario. Developing exploration vectors towards Sudbury breccia- hosted Cu-Ni-PGE mineralization is inhibited by an insufficient understanding of the relative contributions of footwall lithologies versus impact melt. By combining whole-rock geochemistry, field observations, statistical modelling and petrography, this study has determined that Sudbury breccia is a parautochthonous shock melt, which does not require a melt sheet contribution. -
Instability of the Southern Canadian Shield During the Late Proterozoic 2 3 Kalin T
1 Instability of the southern Canadian Shield during the late Proterozoic 2 3 Kalin T. McDannella,b*, Peter K. Zeitlera, and David A. Schneiderc 4 5 aDepartment of Earth and Environmental Sciences, Lehigh University, 1 W. Packer Ave. Bethlehem PA, 18015 USA 6 7 bGeological Survey of Canada, Natural Resources Canada, 3303 – 33 St NW Calgary AB, T2L 2A7 Canada 8 9 cDepartment of Earth & Environmental Sciences, University of Ottawa, 25 Templeton Ave., Ottawa ON, K1N 6N5 10 Canada 11 12 *corresponding author: [email protected]; [email protected] 13 14 ABSTRACT 15 Cratons are generally considered to comprise lithosphere that has remained tectonically 16 quiescent for billions of years. Direct evidence for stability is mainly founded in the Phanerozoic 17 sedimentary record and low-temperature thermochronology, but for extensive parts of Canada, 18 earlier stability has been inferred due to the lack of an extensive rock record in both time and 19 space. We used 40Ar/39Ar multi-diffusion domain (MDD) analysis of K-feldspar to constrain 20 cratonic thermal histories across an intermediate (~150-350°C) temperature range in an attempt 21 to link published high-temperature geochronology that resolves the timing of orogenesis and 22 metamorphism with lower-temperature data suited for upper-crustal burial and unroofing 23 histories. This work is focused on understanding the transition from Archean-Paleoproterozoic 24 crustal growth to later intervals of stability, and how uninterrupted that record is throughout 25 Earth’s Proterozoic “Middle Age.” Intermediate-temperature thermal histories of cratonic rocks 26 at well-constrained localities within the southern Canadian Shield of North America challenge 27 the stability worldview because our data indicate that these rocks were at elevated temperatures 28 in the Proterozoic. -
Magmatism of the Yangtze Craton, South China, As Revealed by Modern River Detrital Zircons
Gondwana Research 42 (2017) 1–12 Contents lists available at ScienceDirect Gondwana Research journal homepage: www.elsevier.com/locate/gr Widespread Neoarchean (~2.7–2.6 Ga) magmatism of the Yangtze craton, South China, as revealed by modern river detrital zircons Peng-Yuan Han, Jing-Liang Guo ⁎, Kang Chen, Hua Huang, Ke-Qing Zong, Yong-Sheng Liu, Zhao-Chu Hu, Shan Gao 1 State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China article info abstract Article history: The Kongling Terrane, which is the Archean nucleus of the Yangtze craton, preserves Paleoarchean-Proterozoic Received 11 February 2016 rocks as old as 3.45 Ga. However, the dominant stage of formation of this Archean terrane remains unclear. In Received in revised form 6 August 2016 this paper, U-Pb and Lu-Hf isotopes of detrital zircons from two rivers and one stream in the northern part of Accepted 2 September 2016 the Kongling Terrane were studied by LA-ICP-MS and LA-MC-ICP-MS, respectively. These zircons show compli- Available online 11 October 2016 cated internal structures in cathodoluminescence images, but the majority of them have linear or oscillatory Handling Editor: S. Kwon zoning patterns, indicating magmatic origins. In general, the detrital zircons from these three local rivers show similar U-Pb age distributions. Together, they yield age peaks at 3.3–3.1 Ga (5%), 3.0–2.8 Ga (18%), 2.7–2.6 Ga Keywords: (30%), 2.6–2.2 Ga (15%), 2.0–1.9 Ga (27%), 1.9–1.7 Ga (1%), 1.7–1.5 Ga (2%), and 1.0–0.8 Ga (1%).