| Reference Type | Journal (article/letter/editorial) |
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| Title | Magnetic Measurements Over Darnley Bay, N.W.T. |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Riddihough, R. P. | Author |
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| Haines, G. V. | Author |
| Year | 1972 (August 1) | Volume | 9 |
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| Issue | 8 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e72-081Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 473424 | Long-form Identifier | mindat:1:5:473424:0 |
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| GUID | 0 |
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| Full Reference | Riddihough, R. P., Haines, G. V. (1972) Magnetic Measurements Over Darnley Bay, N.W.T. Canadian Journal of Earth Sciences, 9 (8) 972-978 doi:10.1139/e72-081 |
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| Plain Text | Riddihough, R. P., Haines, G. V. (1972) Magnetic Measurements Over Darnley Bay, N.W.T. Canadian Journal of Earth Sciences, 9 (8) 972-978 doi:10.1139/e72-081 |
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| In | (1972, August) Canadian Journal of Earth Sciences Vol. 9 (8) Canadian Science Publishing |
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| Abstract/Notes | Five high level, 3-component, magnetic profiles outline a large magnetic anomaly approximately coincident with the previously observed, 130 mgal, positive gravity anomaly. Three-dimensional interpretations of the magnetic data establish the major dimensions of the source body but do not distinguish between a normal and inverted conical shape. Directions of magnetization derived from the interpretations suggest that the body is geologically related to the Precambrian Franklin Diabases. |
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