Zobrazeno 1 - 10
of 103
pro vyhledávání: '"H. H. Read"'
Autor:
H. H. Read
Publikováno v:
Geological Magazine. 71:302-317
The Chapters on the Geology of Scotland, by B. N. Peach and John Home, reveals very clearly the complete divergence in the views of these two masters concerning certain fundamental problems of the Moine Series. Peach (1, pp. 199–200) regards the Mo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f2ac2cb55ae001f7d650b40e7a6c1520
https://doi.org/10.1017/s0016756800093389
https://doi.org/10.1017/s0016756800093389
Autor:
W. S. Pitcher, H. H. Read
Publikováno v:
The Journal of Geology. 71:261-296
Seven high-level granites in Donegal got into position by various mechanisms involving reactive emplacement, radial distension of the country rocks, lateral wedging and horizontal stretching of the latter, and permitted emplacement through cauldron s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e25826b4b2e001d2ff6d6410e668aa21
https://doi.org/10.1086/626902
https://doi.org/10.1086/626902
Autor:
H. H. Read
Publikováno v:
Mineralogical Magazine and Journal of the Mineralogical Society. 23:317-328
Among the many beautiful rocks of Unst, the most northerly of the Shetlands, is one composed of rosettes of pale blue kyanite set in a base of glassy quartz. This rock was mentioned by Heddle, but has never been described, nor have its genetic relati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5ea7a275762572f7ac1f6cf0fc86f38f
https://doi.org/10.1180/minmag.1933.023.140.04
https://doi.org/10.1180/minmag.1933.023.140.04
Autor:
H. H. Read
Publikováno v:
Transactions of the Royal Society of Edinburgh. 55:755-772
A glance at a geological map of Middle Deeside shows that below Cambus O'May the valley is floored by a belt of metamorphic rocks flanked on both north and south by high hills of Younger Granite, of a date later than the regional metamorphism. The ar
Externí odkaz:
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https://doi.org/10.1017/s0080456800013375
https://doi.org/10.1017/s0080456800013375
Autor:
H. H. Read
Publikováno v:
Geological Journal. 2:653-683
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5490b072533aa228af1960b91925714d
https://doi.org/10.1002/gj.3350020408
https://doi.org/10.1002/gj.3350020408
Autor:
H. H. Read
Publikováno v:
Geological Magazine. 63:422-429
The Geological Survey has recently formed a very extensive collection of the dyke-rocks of Galloway. This collection was made mainly by Mr. Robert Eckford, and, to a less extent, by Mr. Wm. Manson. One or more specimens were taken of practically ever
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d3dc9b2fb478699a51afd6465560eb92
https://doi.org/10.1017/s0016756800085162
https://doi.org/10.1017/s0016756800085162
Autor:
H. H. Read
Publikováno v:
Geological Magazine. 6:364-371
The field-work upon which this communication is based was carried out in 1917 and 1918, in preparation for the Geological Survey map of Sheet 86 (Huntly).
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::25b6751c1d45bccc0340f480c7f2502f
https://doi.org/10.1017/s0016756800201520
https://doi.org/10.1017/s0016756800201520
Autor:
H. H. Read
Publikováno v:
Geological Magazine. 66:547-552
In my account of the petrology of the Arnage district of Aberdeenshire, there appeared a description, figure, and analysis of a cordierite-spinel-hornfels from Gallowhill Brae, Arnage. This rock is composed almost entirely of cordierite, with only an
Externí odkaz:
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https://doi.org/10.1017/s0016756800102432
https://doi.org/10.1017/s0016756800102432
Autor:
Yu-Chi Cheng, H. H. Read
Publikováno v:
Quarterly Journal of the Geological Society. 99:107-154
Summary The Migmatization of pelitic, semipelitic, siliceous and hornblendic (Durcha type) rocks of the Moine Series is a record of a lengthy series of metasomatic changes brought about by the activity of alkaline solutions. Pelitic gneisses are conv
Externí odkaz:
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https://doi.org/10.1144/gsl.jgs.1943.099.01-04.10
https://doi.org/10.1144/gsl.jgs.1943.099.01-04.10