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11. |
Occurrence of ignimbrite in the Shag Valley, North-east Otago |
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New Zealand Journal of Geology and Geophysics,
Volume 2,
Issue 2,
1959,
Page 380-384
A. Steiner,
D. A. Brown,
A. J. R. White,
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摘要:
Petrography of the acid igneous rock of the Shag Valley in North-east Otago, previously classified as a quartz porphyry, indicates that this rock is an ignimbrite. Formerly described as a dyke, the Shag Valley rock is now considered to be a surface rock interbedded with coal measures of Upper Senonian age, and is the first occurrence of ignimbrite described from the South Tsland of New Zealand.
ISSN:0028-8306
DOI:10.1080/00288306.1959.10417656
出版商:Taylor & Francis Group
年代:1959
数据来源: Taylor
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12. |
Radioactive boulders in Hawks Crag Breccia |
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New Zealand Journal of Geology and Geophysics,
Volume 2,
Issue 2,
1959,
Page 385-393
A. Wodzicki,
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摘要:
Several radioactive hornfels and granite boulders have been found scattered through the Hawks Crag Breccia in the Big River and Lower Buller Gorge areas., Uraninite has been identified in the radioactive biotite hornfels from the Lower Buller Gorge. An unidentified, iron-rich, uranium-bearing mineral occurs in the radioactive biotite hornfels from the Big River area. The radioactivity in the biotite granite from the Big River area is concentrated in the zircon and apatite inclusions and to a lesser extent in the biotite.
ISSN:0028-8306
DOI:10.1080/00288306.1959.10417657
出版商:Taylor & Francis Group
年代:1959
数据来源: Taylor
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13. |
Some field and petrographic features of American and New Zealand ignimbrites |
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New Zealand Journal of Geology and Geophysics,
Volume 2,
Issue 2,
1959,
Page 394-411
R. C. Martin,
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摘要:
In a study of some New Zealand and American ignimbrites (welded tuffs or ash-flow deposits), close similarities were found in the lithology and topographic relations of the deposits.
ISSN:0028-8306
DOI:10.1080/00288306.1959.10417658
出版商:Taylor & Francis Group
年代:1959
数据来源: Taylor
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14. |
Petrography of the Whakapapanui Gorge Andesites, Mount Ruapehu |
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New Zealand Journal of Geology and Geophysics,
Volume 2,
Issue 2,
1959,
Page 412-420
B. E. O'Shea,
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PDF (1639KB)
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摘要:
Petrological study of the andesite lavas exposed in Whakapapanui Gorge on the northern slopes of Mt. Ruapehu reveals constant mineralogical composition of flows. All are porphyritic andesites with phenocrysts of plagioclase, hypersthene, and augite set in a hyalopilitic groundmass. Slight variations in texture sometimes occur between and within flows of lava.
ISSN:0028-8306
DOI:10.1080/00288306.1959.10417659
出版商:Taylor & Francis Group
年代:1959
数据来源: Taylor
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