2 edition of A seismic survey in the Canadian Shield. found in the catalog.
A seismic survey in the Canadian Shield.
John Humphrey Hodgson
Written in English
Thesis (PhD) - University of Toronto, 1951.
|The Physical Object|
As part of Metal Earth project, a total of km long 2D seismic lines are gathered across the Canadian Shield in Quebec and Ontario Provinces in Fall The seismic data were collected with long offsets and various spatial sampling scenarios. High resolution 2D/3D seismic surveys performed for the Geological Survey of Canada to advance the use of seismic methods in hard rock environments. Organization: Natural Resources Canada Lithoprobe transect 10 - Eastern Canadian Shield Onshore-Offshore Transect.
Careful measurements of phase velocities in the Canadian shield have been made in the period range 3 to 90 sec for Rayleigh waves and 12 to 60 sec for Love waves by phase correlation of wave trains. The continental Love wave phase velocity data are the first to be reported in the by: During the early Forties the first geophysical surveys (gravity and seismic) were undertaken in selected areas. They led to discovery of the Jumping Pound, Sarcee and Pincher Creek gas fields. A stimulating synthesis of geologic and geophysical data was published by Link (). During the Fifties extensive regional seismic surveys were.
the outline of the 3D seismic survey. The inset shows the tectonic map of the Canadian Shield, including the Trans-Hudson orogen (THO). The black square indicates the location of the study area. Minerals , 9, 4 of 23 Table 1. a The location of the study borehole (Hunt well) and 2D seismic surveys in the dominion land survey (DLS) system of Alberta west of the 4th Meridian. The crooked 2D seismic survey has a profile length of 24 km, whereas the straight seismic survey (not discussed in this paper, Chan ) is 3 km long. Both profiles are (re-)processed Cited by: 4.
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Lithosphere and Canadian Shield Division, Geological Survey of Canada, Observatory Crescent, Ottawa, Ontario K1A 0Y3, Canada and processing of the seismic reflection and refraction data available in the deep basins and major ridges in the Arctic Ocean and briefly discusses the salient geological results by region.
No seismic profiling. Summary. In –88 a deep seismic reflection survey was conducted over the Kapuskasing structural zone (KSZ) in the Canadian shield as a part of the LITHOPROBE Project.
Approximately km of vibroseis data were acquired along 9 profiles which crossed the boundaries between the KSZ and Val Rita Block to the west and between the KSZ and Cited by: 5. Proterozoic orogens of the northeastern Canadian Shield: new information from the Lithoprobe ECSOOT crustal reflection seismic survey Jeremy Hall, Richard J.
Wardle, Charles F. Gower, Andrew Kerr, Kevin Coflin, Charlotte E. Keen, Peter CarrollCited by: Initial seismic observations from a deep borehole drilled into the Canadian Shield in northeast Alberta. and a limited 3D seismic survey.
In this study, the data from the multi-azimuthal. Seismic data from new networks in the Hudson Bay region of the Canadian Shield, where the Precambrian geological record spans more than 2 billion years, offer fresh scope to address this problem.
Using receiver function analyses we show that the crust of the Rae domain. From the Canadian shield region, ,[16,17] documented the potential of seismic methods for hard rock mineral exploration to a depth range of about m the limit at which modern mining methods are capable of economically extracting ore.
[4, 5, 14, 15 ]Author: Okan Evans Onojasun. CSZ earthquakes occur in the Canadian Shield, between the surface and 30 km depth, beneath Logan's line and the Appalachians.
On average, an earthquake occurs in the Charlevoix region every day and a half. More information. View seismicity during the last 30 days.
publications. Lower St. mic surveys focussed primarily on deep mineral exploration: the Oryx survey in the Witwatersrand Basin, South Africa (De Wet and Hall, ); the Trill survey in Sudbury, Canada (Milkereit et al., this volume); and the Matagami survey, in the northern Abitibi subprovince of the Canadian shield (Adam et al., this volume).
These three surveys sample. Seismic survey, method of investigating subterranean structure, particularly as related to exploration for petroleum, natural gas, and mineral deposits.
The technique is based on determining the time interval that elapses between the initiation of a seismic wave at a selected shot point. A full suite of geophysical logs, including nuclear, electric, acoustic transit-time, acoustic waveform, and acoustic televiewer logs, and high-resolution flowmeter measurements have been used to investigate the lithologic and hydrologic properties of three igneous plutons located on the southern margin of the Canadian shield.
GEOPHYSICAL WELL-LOGANALYSIS IN CHARACTERIZING THE HYDROLOGY OF CRYSTALLINE ROCKS OF THE CANADIAN SHIELD by F.L. Paillet Borehole Geophysics Research Project Water Resources Division U. Geological Survey Denver, Colorado ABSTRACT A full suiteofgeophysical logs, including nuclear, electric, acoustic transit-time,acous.
• Regional seismic surveys in hard rock environment a) Lithoprobe (Canada) b) COCORP (the USA) c) AGSO (Australia) d) Europrobe (Europe) e) National Geophysics Program (SouthAfrica) • Canada: exploration done by industry, academic research, TGI programs • Highlight: acquiring 3D dataset: Sudbury, Brunswick No.
6, Half-mile Lake, FlinFile Size: 4MB. NOTICE: The Canadian National Seismograph Network (CNSN) is undergoing equipment upgrades over the next few years. The seimograms from some stations may not be viewable on the web although we continue to acquire and process data from them.
Two high‐resolution surveys in the Swayze area, a poorly endowed part of the western Abitibi greenstone belt, served as pioneer surveys with which to better understand subsurface geology and design a strategy to process other surveys in the near future.
Swayze seismic data were acquired with crooked survey geometries along : Saeid Cheraghi, Mostafa Naghizadeh, David Snyder, Rasmus Haugaard, Thomas Gemmell. Whether or not plate tectonic processes operated on a younger, hotter Earth remains ambiguous. Seismic data from new networks in the Hudson Bay region Cited by: Access the LITHOPROBE seismic and MT data archive: Seismic reflection, refraciton and magnetotelluric (MT) data collected by LITHOPROBE in its 10 transects across Canada now are archived at the Seismology and Electromagnetic Section of the Geological Survey of Canada.
These data are available for interested companies, institutions and individuals. Green areas shows location of the Abitibi subprovince of the Canadian shield, one of the most important mining regions in the world. Lithoprobe Sincethe Geological Survey of Canada, in collaboration with industry, has undertaken a systematic program to evaluate the use of seismic-reflection methods for mineral exploration.
Ambient seismic noise tomography of Canada and adjacent regions: Part I. Crustal structures Honn Kao,1,2 Yannik Behr,3,4 Claire A.
Currie,5 Roy Hyndman,1,2 John Townend,4 Fan-Chi Lin,6 Michael H. Ritzwoller,7 Shao-Ju Shan,1 and Jiangheng He1 Received 17 July ; revised 25 October ; accepted 29 October ; published 21 November The availability of a deep borehole offers an unprecedented opportunity to correlate surface seismic data to borehole measurements in the metamorphic rocks of northeastern Alberta, Canada.
As part of the feasibility study for the development of engineered geothermal systems (EGS) in Alberta under the Helmholtz-Alberta Initiative (HAI), this project provides a detailed subsurface Cited by: 5. The Precambrian Canadian Shield and the bounding platforms of North America's interior comprise the core of Laurentia (Hammer et al., ).
Several distinct geological provinces brought together during a series of Paleoproterozoic orogens make up the Canadian Shield (Hoffman,Fig. The largest of these provinces, and the world's Cited by: 6. Geological map of the Chisel basin with a SW–NE-oriented cross section of the Lalor volcanogenic massive sulﬁde (VMS) deposit generalized after .
The rectangle on the map shows the outline of the 3D seismic survey. The inset shows the tectonic map of the Canadian Shield, including the Trans-Hudson orogen (THO).Cited by: 1.Seismic reflection and refraction images indicate north-dipping structures, interpreted as a stack of discrete, 10 to 15 km thick terranes.
A slab of high-velocity material, possibly representing subcreted oceanic lithosphere, as well as Moho offsets, support a model of progressive accretion through plate-tectonic-like processes. Regional and high‐resolution seismic surveys were acquired and studied within the Abitibi greenstone belt (Fig.
1) by the Lithoprobe project in Canada during –; the main objective of these surveys was to better understand architecture and evolution of the crust (Clowes ).Author: Saeid Cheraghi, Mostafa Naghizadeh, David Snyder, Rasmus Haugaard, Thomas Gemmell.