(1913) VI.—The Petrology of Arran. Geological Magazine, S. 5 Vol. 10 (7) 305-309 doi:10.1017/s0016756800126743
Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | VI.—The Petrology of Arran | ||
Journal | Geological Magazine | ||
Year | 1913 (July) | Series:Volume | 5:10 |
Page(s) | 305-309 | Issue | 7 |
Publisher | Cambridge University Press (CUP) | ||
DOI | doi:10.1017/s0016756800126743 | ||
Mindat Ref. ID | 279559 | Long-form Identifier | mindat:1:5:279559:5 |
GUID | 696c46dc-9373-4af4-945a-5e35c4eb50bc | ||
Full Reference | (1913) VI.—The Petrology of Arran. Geological Magazine, S. 5 Vol. 10 (7) 305-309 doi:10.1017/s0016756800126743 | ||
Plain Text | (1913) VI.—The Petrology of Arran. Geological Magazine, S. 5 Vol. 10 (7) 305-309 doi:10.1017/s0016756800126743 | ||
In | (1913, July) Geological Magazine S. 5 Vol. 10 (7) Cambridge University Press (CUP) | ||
Abstract/Notes | The Riebeckite-Orthophyre of the Holy Isle.—Four Occuxrences of acid and sub-acid igneous rocks containing the rare soda-amphibole riebeckite have been recognized in Great Britain, of which that of Ailsa Craig is the best known. The occurrences of Ailsa Craig and Mynydd Mawr, Carnarvonshire, are riebeckite-microgranites or paisanites. They contain ragged moss-like areas of riebeckite, together with microphenocrysts of quartz and alkalifelspar, in a microcrystalline groundmass of quartz and felspar. Riebeckite was also found by Dr. Teall in the granophyre of Meall Dearg and the neighbouring area of Druim an Eidhne, Skye. Harker described the riebeckite in these rocks as occurring in two forms, one having the usual ragged, sponge-like appearance, and the other being idiomorphic, the faces in the prism zone being well-defined, but with irregular terminations. The fourth occurrence differs somewhat from the others. This rock occurs as an intrusion into the Upper Old Red Sandstone, or Calciferous Sandstone of Easter Eildon Hill, Melrose, and was described by Barron as riebeckite-trachyte or phonolite. It consists principally of sanidine, occurring both as microphenocrysts and in the groundmass, with interstitial patches of riebeckite, and a little nepheline. Harker describes the rock as an orthophyre. |
References Listed
These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.
Q.J.G.S. xxx, 563, 1874 | |
(1895) Tscherm. Min. Petr. Mitth. xiv, 463 | |
(1910) The Geology of the Neighbourhood of Edinburgh , 299 | |
(1911) The Geology of Knapdale, Jura, and North Kintyre , 117 | |
(1911) The Geology of Colonsay and Oronsay , 41 | |
Geology of North Arran, etc., p. 91. | |
Tyrrell , Geol. Mag. (V), IX, 124, 1912 | |
(1908) Petrology for Students , 129 | |
Not Yet Imported: BMJ - journal-article : 10.1136/bmj.1.1726.219-a If you would like this item imported into the Digital Library, please contact us quoting Journal ID 9994 | |
(1911) The Geology of Knapdale, Jura, and North Kintyre , 116 | |
(1903) The Geology of North Arran, South Bute, and the Cumbraes , 70 | |
(1910) Summ. Prog. Oeol. Surv. for 1909 , 52 | |
Geol. MAG., 1896, p. 376. | |
(1904) Tertiary Igneous Bocks of Skye , 158 | |
(1911) The Geology of Colonsay and Oronsay, with Part of the Ross of Mull , 41 | |
(1903) The Geology of North Arran, South Bute, and the Cumbraes , 112 | |
Harker (1889) Bala Vole. Ser. Carnarvon , 50 |
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