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Wednesday, May 20, 2020 | History

2 edition of LithoProbe Western Superior Transect Third Annual Workshop found in the catalog.

LithoProbe Western Superior Transect Third Annual Workshop

Western Superior Transect Workshop (3rd 1997 Toronto, Ont.)

LithoProbe Western Superior Transect Third Annual Workshop

April 11-12, 1997

by Western Superior Transect Workshop (3rd 1997 Toronto, Ont.)

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  • 37 Currently reading

Published by Lithoprobe Secretariat, University of British Columbia in [Vancouver, B.C.?] .
Written in English

    Subjects:
  • Basins (Geology) -- Superior, Lake, Region -- Congresses.,
  • Basins (Geology) -- Ontario -- Congresses.,
  • Cratons -- Superior, Lake, Region -- Congresses.,
  • Cratons -- Ontario -- Congresses.,
  • Geology -- Superior, Lake, Region -- Congresses.,
  • Geology -- Ontario -- Congresses.,
  • Geology, Stratigraphic -- Archean -- Congresses.,
  • Geology, Structural -- Superior, Lake, Region -- Congresses.,
  • Geology, Structural -- Ontario -- Congresses.

  • Edition Notes

    Other titlesWestern Superior Transect Third Annual Workshop, Western Superior LithoProbe Third Annual Workshop
    Statement[editors] Rob Harrap, Herb Helmstaedt.
    SeriesLithoprobe report -- no. 63
    ContributionsHarrap, Robin Michael, 1961-, Helmstaedt, Herb.
    Classifications
    LC ClassificationsQE191 .W48 1997
    The Physical Object
    Pagination108 p. :
    Number of Pages108
    ID Numbers
    Open LibraryOL18788401M

    Lerner-Lam (), "Where is the western edge of the North American Craton?", AGU Fall Meeting Abstract 74 (43) Chen, W., W. Chi, D. Dolenc, B. Kuo, C. Lin, J.A. Collins (), "Typhoon-induced microseisms recorded offshore and onland Western Pacific regions", EOS Transactions, AGU Fall Meeting Supplement Abstract AN. no category - annual institute on lake superior geology.

    Categories. Baby & children Computers & electronics Entertainment & hobby. ELSEVIER Precambrian Research 91 () Prernmbrinn Resenrth Archean magmatism and deformation were not products of plate tectonics Warren B. Hamilton * Department of Geophysics, Colorado School of Mines, Golden, C, USA Received 4 October ; accepted 30 June Abstract The granite-and-greenstone terrains that dominate upper crust formed from about to Cited by:

    LITHOPROBE seismic profiling, the main pulse of the Trans-Hudson Orogen is interpreted to have. resulted from the ca. to Ga continent-continent collision of three Archean cratons, the. Superior, Hearne, and Sask cratons, with resultant trapping of juvenile intraoceanic rocks in the. The SBS is a relatively small (4 kin) reflector lying at to 6 1 Now at Dept. of Physics, New Mexico State University, Las Cruces, New Mexico 2 Now at GEOMAR, Wischhofstrasse , K F. R. G. Continental Lithosphere: Deep Seismic Reflections Geodynamics 22 o American Geophysical Union sec traveltime (about 16 km.


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LithoProbe Western Superior Transect Third Annual Workshop by Western Superior Transect Workshop (3rd 1997 Toronto, Ont.) Download PDF EPUB FB2

Report of Annual Workshop, The University of British Columbia, LITHOPROBE Rep pp Stauffer, M.R.,Manikewan: an Early Proterozoic ocean in central. the end of the third year. Lithoprobe was launched as a. held an annual workshop during its active period, The most recent transect, Western Superior.

Control of the western continental margin of North America by the Cordilleran Fairweather-Queen Charlotte-Wallowa fault system; in: F. Cook and P. Erdmer (comps.), Slave-Northern Cordillera Lithospheric Evolution (SNORCLE) Transect and Cordilleran Tectonics Workshop Meeting; Lithoprobe Report #56, p.

Lyatsky, H.V. and Dietrich, J.R. Abercrombie, R.E. (), "The magnitude-frequency distribution of earthquakes recorded with deep seismometers at Cajon Pass, Southern California", Tectonophysics () Abercrombie, R.E.

(), "Near-surface attenuation and site effects from comparison of surface and deep borehole recordings", Bulletin of the Seismological Society of America 87 (3) Al-Aasm, I.S., Z. Lu, and T. White. Evolution of pore fluids and dolomitization of Mississippian carbonates of western Canada sedimentary basin: petrologic and chemical constraints.

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This feature is interpreted to be Superior Province lithosphere and the corresponding N85°E geoelectric strike to be associated with the fabric of the Superior Province.

The base of the resistor reaches depths of km on two of the three MT profiles north of Lake Ontario and this depth is interpreted to be the base of the by: Annual Reviews: Hydrologic processes from catchment to continental scales: Annual Reviews, Global: Book - ad, Hydrology, geomorphology, brine: DS Annual Reviews: Origin of planets and life: Annual Reviews, Global: Book - ad, Planets and Life: DS Arnold, R.H.

Interpretation of airphotos and remotely sensed imagery. Introduction. The Superior Province is the largest Archean craton on Earth. It preserves an extended period of crustal growth, from ca. to ca. Ga (Card,Percival et al.,Percival et al.,Skulski et al., a), and holds clues to the origin of continental crust and the nature of ancient tectonic from the craton has provided the best evidence for Cited by: 5.

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