| Reference Type | Journal (article/letter/editorial) |
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| Title | Megalineament in southeastern Alaska marks southwest edge of Coast Range batholithic complex |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Brew, David A. | Author |
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| Ford, Arthur B. | Author |
| Year | 1978 (November 1) | Volume | 15 |
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| Issue | 11 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e78-184Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 475652 | Long-form Identifier | mindat:1:5:475652:5 |
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| GUID | 0 |
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| Full Reference | Brew, David A., Ford, Arthur B. (1978) Megalineament in southeastern Alaska marks southwest edge of Coast Range batholithic complex. Canadian Journal of Earth Sciences, 15 (11) 1763-1772 doi:10.1139/e78-184 |
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| Plain Text | Brew, David A., Ford, Arthur B. (1978) Megalineament in southeastern Alaska marks southwest edge of Coast Range batholithic complex. Canadian Journal of Earth Sciences, 15 (11) 1763-1772 doi:10.1139/e78-184 |
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| In | (1978, November) Canadian Journal of Earth Sciences Vol. 15 (11) Canadian Science Publishing |
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| Abstract/Notes | The Coast Range megalineament is a prominent, nearly continuous topographic and structural feature that extends southeastward about 550 km (330 mi) from its junction with the Chatham Strait – Lynn Canal fault at Point Sherman to Tongass Passage near the mouth of Pearse Canal where it leaves southeastern Alaska. It probably extends still further southeastward into British Columbia along Work Channel and Chatham Sound – Grenville Channel.The megalineament is a zone a few hundred metres to 10 km (6 mi) wide in which closely spaced joints, foliation, compositional layering, and small faults define the megalineament trend. The zone usually coincides with topographic depressions apparently caused by selective fluvial and glacial erosion of the less resistant rocks of the zone.Studies in the Juneau, Endicott Arm, and Behm Canal areas indicate that the megalineament (1) is locally the site of lateral and (or) vertical separations of no greater than several kilometres; (2) does not mark a major structural or metamorphic discontinuity in the near-surface rocks; (3) may be located near a pre-metamorphic and pre-intrusive discontinuity; (4) is consistently associated with and parallel to steep gradients in both the gravity and aeromagnetic fields; and (5) probably is the surface expression of the western contact, at depth, of the intrusive rocks and gneisses of the Coast Range batholithic complex with the schists to the southwest. |
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