| Reference Type | Journal (article/letter/editorial) |
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| Title | Tectonic Features of the Hecla Hook Formation to the South of St. Jonsfjord, Vestspitsbergen |
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| Journal | Geological Magazine |
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| Authors | Weiss, L. E. | Author |
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| Year | 1953 (August) | Volume | 90 |
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| Issue | 4 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800065468 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 248286 | Long-form Identifier | mindat:1:5:248286:0 |
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| GUID | 0 |
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| Full Reference | Weiss, L. E. (1953) Tectonic Features of the Hecla Hook Formation to the South of St. Jonsfjord, Vestspitsbergen. Geological Magazine, 90 (4) 273-286 doi:10.1017/s0016756800065468 |
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| Plain Text | Weiss, L. E. (1953) Tectonic Features of the Hecla Hook Formation to the South of St. Jonsfjord, Vestspitsbergen. Geological Magazine, 90 (4) 273-286 doi:10.1017/s0016756800065468 |
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| In | (1953, August) Geological Magazine Vol. 90 (4) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractA structural study of rocks of the Hecla Hook formation in the area of Forlandsundet of Vestspitsbergen reveals the presence of two B–axes. The earlier (B1) trends roughly east–west and affects only the Hecla Hook formation; the later axis (B2) trends roughly north–south, and affects also rocks of Carboniferous age. It is suggested that B1 is the main “Caledonian” axis in this area, and that B2 and the roughly north–south “grain” of the rocks concerned are Lower Tertiary phenomena. |
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These are possibly similar items as determined by title/reference text matching only.
