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- W1963595110 abstract "In my paper on “The Age of the Newer Gneissic Rocks of the Northern Highlands,” I suggested that a study of the old rocks of Ireland would probably aid in connecting the Scottish types with those of South Britain; and, in the summer of 1884, I visited the north of Ireland to ascertain how far my suspicion was justified by the facts. As Professor Hull had announced the discovery of Laurentian gneiss in the same area, I included the relations between this group and the schists in my investigation. A continuance of stormy weather prevented the completion of my plans; but I obtained satisfactory proof of the nature and relations of the chief granitoid mass, and collected partial material for the study of the schistose rocks. As the result of a month9s work, I came to the conclusion that the schistose rocks of Northern Donegal were separable into two groups, and that the so-called “Laurentian” was merely a mass of granite intrusive in the older of them. The President (Professor Bonney), with his usual kindness, has examined fifty-five microscopic sections of Irish rocks, and he permits me to use at my discretion the rough notes which he has furnished. It is to be regretted that pressure of other work has prevented him from undertaking a more elaborate investigation. I. TheGranite. 1. State of Previous Opinion. Mr. R. H. Scott, F.R.S., claims a metamorphic origin for this rock. Mr. E. H. Blake takes the same view. In a subsequent paper" @default.
- W1963595110 created "2016-06-24" @default.
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- W1963595110 date "1885-02-01" @default.
- W1963595110 modified "2023-09-25" @default.
- W1963595110 title "On the Granitic and Schistose Rocks of Northern Donegal" @default.
- W1963595110 doi "https://doi.org/10.1144/gsl.jgs.1885.041.01-04.26" @default.
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