| Reference Type | Journal (article/letter/editorial) |
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| Title | II.—The Structure and Later Geological History of New Zealand |
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| Journal | Geological Magazine |
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| Year | 1916 (June) | Series:Volume | 6:3 |
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| Issue | 6 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800201313 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 264774 | Long-form Identifier | mindat:1:5:264774:0 |
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| GUID | 0 |
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| Full Reference | (1916) II.—The Structure and Later Geological History of New Zealand. Geological Magazine, S. 6 Vol. 3 (6) 243-249 doi:10.1017/s0016756800201313 |
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| Plain Text | (1916) II.—The Structure and Later Geological History of New Zealand. Geological Magazine, S. 6 Vol. 3 (6) 243-249 doi:10.1017/s0016756800201313 |
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| In | (1916, June) Geological Magazine S. 6 Vol. 3 (6) Cambridge University Press (CUP) |
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| Abstract/Notes | As is well known, the skeleton or oldermass of New Zealand is largely composed of a mass of deformed sedimentary rocks, the precise ages of the members of which are in doubt but do not affect the problem under consideration. The most profound deformation of this vast sedimentary group took place in late Jurassic or early Cretaceous times during what may be termed the “Mesozoic orogenic period”, when probably a great mountain range came into existence. |
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These are possibly similar items as determined by title/reference text matching only.
