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单词 schaalstein
释义

schaalsteinschalsteinn.

/ˈʃɑːlʃtʌɪn/
Forms: Also schaallstein, and partly translated as schaalstone /ˈʃɑːlstəʊn/.
Etymology: German, < schale (formerly schaale ) skin, shell + stein stone. See also shale n.2 and scale n.1
Geology.
a. = wollastonite n. Obsolete.
ΘΚΠ
the world > the earth > minerals > types of mineral > silicates > inosilicates single chain > [noun] > pyroxenoid > wollastonite
schaalstein1804
table spar1814
wollastonite1823
grammite1826
pseudowollastonite1905
parawollastonite1935
1804 R. Jameson Syst. Mineral. I. 519 (heading) Schaalstein.—Werner.
1804 R. Jameson Syst. Mineral. I. 520 It is named schaalstone, which in German intimates that it is composed of lamellar distinct concretions. I have not been able to find any English word synonymous to the German, so that I am under the necessity of adopting it.
1819 W. Phillips Elem. Introd. Mineral. (ed. 2) Index 300/1 Schaallstein.
1836 T. Thomson Outl. Mineral. I. 129 Bisilicate of Lime. Table spar, schaalstein, grammite, wollastonite of Hauy.
b. Any of several basic or calcareous tuffaceous rocks, usually laminated in structure, affected by low-grade metamorphism; a slaty or sheared greenstone.
ΘΚΠ
the world > the earth > structure of the earth > constituent materials > rock > sedimentary rock > [noun] > calcareous tuff
tophus1555
calcareous tuff1569
calcareous tufa1811
calc-tuff1822
schaalstein1866
1866 P. H. Lawrence tr. B. von Cotta Rocks Classified ii. iv. 311 Some part at least of what has been called schalstein belongs to the tufa formation.
1879 F. Rutley Stud. Rocks xiii. 248 Schalstein is, according to Gümbel, a tuff, or sedimentary deposit, the material for which has been derived from ‘diabase-eruptions’.
1882 A. Geikie Text-bk. Geol. 165 Schalstein.—Under this name German petrographers have placed a variety of rocks which consist of green, grey, red, or mottled diabase-tuff impregnated with carbonate of lime and mixed with calcareous and argillaceous mud.
1897 A. Geikie Anc. Volcanoes Brit. II. xxix. 36 Some layers of this tuff assume a finely foliated appearance by the development of pale leek-green folia, which show slickensided surfaces parallel with the bedding. The rock then presents one of the usual appearances of schalstein.
1909 W. A. E. Ussher et al. Geol. Country around Bodmin & St. Austell vi. 44 North of Bury Down..the Middle Devonian Slates are associated with schalsteins.
1974 E. Lehmann in G. C. Amstutz Spilites & Spilitic Rocks 23 In the Lahn syncline..of Western Germany, the central rock complex, of upper Middle Devonian and lower Upper Devonian age, consists of so-called ‘schalstein’. Any consistency, however, suggested by that old miner's term, is not reflected in the petrographic character of the rock.
This entry has not yet been fully updated (first published 1982; most recently modified version published online December 2020).
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n.1804
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