Last edited by Dailkis
Tuesday, April 21, 2020 | History

1 edition of Bouger anomaly map : Sudbury Ontario. found in the catalog.

Bouger anomaly map : Sudbury Ontario.

Bouger anomaly map : Sudbury Ontario.

  • 43 Want to read
  • 11 Currently reading

Published by Natural Resources Canada in Ottawa .
Written in English

    Subjects:
  • Geology - Sudbury - Maps,
  • Gravity maps

  • Edition Notes

    SeriesCanada. Geological Survey. Map 138
    The Physical Object
    Pagination1 sheet
    ID Numbers
    Open LibraryOL22068246M


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Bouger anomaly map : Sudbury Ontario. Download PDF EPUB FB2

Regional gravity setting of the Sudbury Structure Bouguer gravity anomaly map of region gridded using The 3D geologic and structural setting of the Sudbury Structure was predicted by an. Metamorphism of the Canadian Shield, Ontario, Canada.

The regional Bouger anomaly map reveals previously unrecognized first-order folds. Interpretation of the Bouger anomaly map also confirms. Abstract. Several new lithotectonic domains have been identified in the buried Precambrian basement of southwestern Ontario.

They are distinguished by differences in rock type as identified from study of drillcore and cuttings and geophysical (primarily aeromagnetic) trends and intensities on published by: The Ontario Mineral Exploration Review (OMER) spring issue features articles on the Ring of Fire, important Ontario mining camps, and so much more.

% Test MAP Sensor Intake Air Boost Pressure Manifold Absolute Druck Sender For Volvo S40 S70 V40 V70 i The Mysterious Hico Structure, Hamilton-Erath Counties, Texas Map of the Hico structure, Hamilton-Erath Counties, Texas She did find weak Bouger gravity anomalies associated with the ring faults associated with the ring graben (Wiberg; Milton ).

Discussion. In contrast, shocked zircons are recognized in Proterozoic deposits (e.g., Ga Vredefort and Ga Sudbury impact structures; Cavosie et al., ; Thomson et al., ). The oldest known shocked mineral is a single tiny (∼ µm) quartz grain in a Ga spherule layer in Australia (Rasmussen and Koeberl, ).

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The arc segments comprising this anomaly consists of tree lines and drainages associated with ring-like troughs, which encircle the central uplift of the Hico structure. On Landsat imagery, the Hico structure is at the center of a subtle 9-km (mile) in diameter circular feature (Wiberg; Milton ).

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