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2 edition of Geology and summary of results from borehole EBL-1 in the east Bull Lake research area (RA-7) Algoma District, Northeastern Ontario found in the catalog.

Geology and summary of results from borehole EBL-1 in the east Bull Lake research area (RA-7) Algoma District, Northeastern Ontario

Atomic Energy of Canada Limited.

Geology and summary of results from borehole EBL-1 in the east Bull Lake research area (RA-7) Algoma District, Northeastern Ontario

by Atomic Energy of Canada Limited.

  • 369 Want to read
  • 24 Currently reading

Published by Atomic Energy of Canada Limited in Ottawa, Ont .
Written in English


Edition Notes

StatementR.B. Ejeckam ... [et al.].
SeriesTechnical record (Atomic Energy of Canada Ltd) -- 409-1
ContributionsEjeckam, R. B.
The Physical Object
Pagination82 p. :
Number of Pages82
ID Numbers
Open LibraryOL20189016M

  Therefore, geophysical logging is very much required to perform after drilling to know actual lithology with accurate depth. The record of any characteristic information with depth in the borehole is known as well log. When sensor is lowered gradually inside the borehole, continuous recording is made, and it is called geophysical log. The Minnesota Geological Survey is a research and service arm of the Newton Horace Winchell School of Earth and Environmental Sciences at the University of Minnesota. It investigates the geology of Minnesota and provides basic public information on the geology of the state. The Survey works with state, county, and regional offices to set up.

Dear all, The following proposal has been received from the 'Geological Information and Modeling' community of the EPOS implementation phase project, who have been working directly with the Geology Data Specification and more specifically, Boreholes. Please post your responses to this proposal here. Thank you and best wishes, Amelia. Results of cross-borehole flow survey at Lac du Bonnet, Manitoba, Canada, indicating distribution Comparison of geophysical measurements of fractures in borehole FSE4 at the Mirror Lake, The measurement of fracture properties in bore­ holes using conventional geophysical logs is shown in.

is one of the world's leading portals to geology and earth science news and information for rocks, minerals, gemstones, energy, volcanoes, earthquakes, careers, geologic hazards, and more. This report describes the regional and site specific geology of the Hanford Sites low-level burial grounds in the East and West Areas. The report incorporates data from boreholes across the entire Areas, integrating the geology of this area into a single framework.


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Geology and summary of results from borehole EBL-1 in the east Bull Lake research area (RA-7) Algoma District, Northeastern Ontario by Atomic Energy of Canada Limited. Download PDF EPUB FB2

Between andseven Earthscope Plate Boundary Observatory (PBO) boreholes ranging in depth from about to feet deep were drilled in and adjacent to the Yellowstone caldera in Yellowstone National Park, for the purpose of installing volcano monitoring instrumentation.

Five of the seven boreholes were equipped with strainmeters, downhole seismometers, and tiltmeters. The East Bull Lake intrusion is a layered basic lopolith of early Aphebian age that intrudes Archean basement rocks at the southern margin of the Superior Province.

It contains at least two magmatic by: PDF | On Jan 1,F L Paillet and others published Geophysical well log analysis of fractured crystalline rocks at East Bull Lake, Ontario, Canada | Find, read and cite all the research you.

Geology Topography As a first step, the elevation of each borehole was determined by locating them on Google Earth. These were then confirmed by GPS readings during site visits.

The elevations for each borehole are shown in Table 4. Table 4: Borehole Location Elevations Borehole Location Elevation (m) Binslawa Baharka Shawees 1 with borehole coordinates and elevations, and geology of the holes. The work is still in progress, as the number of boreholes is large.

There are approximately 3, logs in the archives and the work contained here represents about 3 percent of those geophysical logs. PARTI ANTARAMUT-KURTAN-DZORAGUKH COAL FIELD Study AreaCited by: 1. Sloto, R. A.: Use of Borehole Geophysical Methods to Identify arid Prevent Cross-Contamination \ Borehole Geophysical Methods Caliper, fluid-resistivity, fluid-temperature, natural-gamma, and single-point-resistance logs were run in bore­ holes in the study area to interpret lithostratigraphy, locate.

Johnson, C.D.,Use of a borehole color video camera to identify lithologies, fractures, and borehole conditions in bedrock wells in the Mirror Lake Area, Grafton County, New Hampshire, in U.S.

Geological Survey Toxic Substance Hydrology Program - Proceedings of the Technical Meeting, Colorado Springs, Colorado, SeptemberU.S. The Engineering Geology Field Manual, in conjunction with the Engineering Geology Office Manual, forms the basis for the mutually beneficial exchange of ideas by Reclamation geologists.

Experienced geologists will find useful reminders and new procedures and special tech­ niques, while less experienced engineering geologists and.

The header of this document typically includes summary hole information such as the borehole identifier, location, date and name of the drill foreman. The body of the document contains the downhole log which is a downwards scaled record of the sequence of. The regional geology is represented by Pilbara Block of the Archean Pilbara Craton covering an area of ∼61, sq.

Pilbara Craton consists of a series of east–west trending granite–greenstone terranes of dome-shaped granitic batholiths separated by synclinal belts of metasediments and metavolcanic rocks. The regional basement stratigraphy is collectively called the Pilbara Supergroup.

The Borehole Research Group (BRG) uses downhole geophysical measurements in a wide variety of scientific investigations including sea level variations, paleoceanography, flow of fluids through fractured rock, and thermal and mechanical properties of the ocean's igneous crust and the properties of.

25, 31; Univ. Texas Bull., no. p. 77 and charts. East Mountain shale member of Mineral Wells formation, uppermost formation of Strawn group (revised) in Brazos River Valley area, north-central Texas. [Not recognized in Colorado River Valley.] Chiefly dark bluish gray shale, about feet thick.

Asterisks indicate S-wave velocities based on the logging results, i.e., not identified here. Identified ~t Equivalent linear Prevention Research Institute, Kyoto, on leave from Bureau de Recherches Géologiques et Minières, Orléans.

in Proc. of the Int. Symp. on the Effects of Surface Geology on Seismic Motion, Odawara City, Japan. The present study was designed to test the placer gold potential of the Elliot Lake Group, Ontario, Canada.

Pyritic quartz-pebble conglomerates and conglomeratic sandstones of probable fluvial. Borehole geophysical logging, aquifer tests, and aquifer-isolation (packer) tests were conducted in four supply wells at the former U.S.

Naval Air Warfare Center (NAWC) in Warminster, PA, to identify the depth and yield of water-bearing zones, occurrence of borehole flow, and effect of pumping on nearby wells. The study was conducted as part of an ongoing evaluation of ground-water. The low borehole yielding potential and the high drilling failure rate of the Voltaian sedimentary rocks of Northern Ghana have been of concern to many local hydrogeologists and international donors.

Consequently, several donor-supported projects have been instituted within the last few years with the view to study the hydrogeological characteristics of this ‘difficult’ rock system.

The results and data from this project, if the borehole disposal concept proves feasible, will help DOE make future decisions on the possibility of using deep boreholes for smaller forms of nuclear waste.

What is a borehole record. A record of boreholes, shafts and wells from all forms of drilling and site investigation work. Boreholes range from one metre to several thousand metres deep. Borehole records are produced from a geologist's or surveyor's observations of the rock core extracted from the ground.

The Groningen area, is a well-studied area and it has ∼70 borehole sites, such that it represents an ideal natural laboratory to test the method. We start with an overview of the geological horizons of interest that are sampled by the measurements and some background on constraints on structure from previous studies (Section 2).

Therefore, recent intercollegiate geoscience research efforts, coordinated through the University of Texas Institute for Geophysics Gulf Basin Depositional Synthesis (GBDS) project and the University of Kansas Geology Department, have set out to improve existing early Mesozoic Gulf of Mexico sediment provenance and routing models.

Borehole geophysics is an aspect of geoscience that deals with the vertical analysis of the conditions of the subsurface and its fluid content. It is the technique employed in order to have a firsthand well evaluation in the exploration for hydrocarbons.

One of the main results of Borehole Geophysical experiment is the Time to Depth relation curve.At the full extent, scale geology is displayed. Zoom in to switch to 1: 50 scale geology. The scale of the currently displayed geology is shown. Zooming in too far will cause the geology to switch off entirely.

These scale levels are required to view boreholes in the borehole scans mode.Geophysical borehole logging is a cost effective way of providing vital subsurface information required by geoscientists in groundwater, environmental, mineral and geotechnical investigations.

In newly-drilled boreholes geophysical logging is used. to guide the design of the borehole and its completion (construction logging).