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- W2016097891 abstract "In a paper published in the Devonshire Transactions for 1888 (p. 215), Mr. Somervail suggests the identity of the chlorite schists of South Devon with certain rocks to the northward. As this hypothesis (could it be established) would have a most important bearing on subjects of controversy, I took the opportunity in a few days this winter, to visit and collect from these localities, including the dyke nearest to Toreross. I was not rewarded by finding any striking similarity to the metamorphic rocks of the south. In that series, the chlorite schists consist of clear and definite crystalline grains, among which I find felspar to be rare and have not yet certainly identified augite—while these northern greenstones are full of broken crystals of both minerals, together with viridite, dust resulting from the crushing, and a small amount of minute secondary hornblende and sericite (?), chlorite being generally rare, and often absent." @default.
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- W2016097891 date "1889-06-01" @default.
- W2016097891 modified "2023-09-27" @default.
- W2016097891 title "VI.—Devonian Greenstones and Chlorite Schists of South Devon" @default.
- W2016097891 doi "https://doi.org/10.1017/s0016756800176290" @default.
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