| 单词 | radiolite | 
| 释义 | radioliten. Now rare.  1.  Palaeontology. A rudist bivalve mollusc of the Cretaceous genus  Radiolites or family  Radiolitidae; = radiolitid n. N.E.D. (1903) gives another sense, for a kind of cephalopod, citing  G. B. Sowerby Man. Conchol. (1839) 91, but this arises from a misreading of Radiolites for Radiolata. ΘΚΠ the world > animals > invertebrates > subkingdom Metazoa > grade Triploblastica or Coelomata > class Pelecypoda or Conchifera > 			[noun]		 > section Siphonida > integro-pallialia > family Hippuritidae > member of hippurite1798 spherulite1834 radiolite1835 rudist1855 rudistid1900 1835    A. Sedgwick  & R. I. Murchison in  Trans. Geol. Soc. 3 365  				A grey limestone..containing..a Radiolite. 1859    D. Page Handbk. Geol. Terms 310  				The Radiolite has an inversely conical under-valve, with a deep straight cavity. 1878    Jrnl. Anthropol. Inst. 7 358  				Below the nummulites, hippurites, and radiolites (Rudisten-Kalk), lies on both sides of the valley, with a sharp dip, a band of limestone..which polishes like marble. 1967    Philos. Trans. 		(Royal Soc.)	 B. 252 94  				Chubb..draws attention to three specimens of the gregarious radiolite Thyrastylon adherens.  2.  Mineralogy. A variety of natrolite occurring in masses with a radiated structure. Chiefly historical. ΚΠ 1835    Rec. Gen. Sci. 1 267  				Radiolite.—Pfaff found this mineral to consist of..Silica...48 Alumina...27 [etc.]. 1868    J. D. Dana Syst. Mineral. 		(ed. 5)	 427  				The radiolite is in radiated masses, and compact fibrous nodules, of a grayish color. 1911    Encycl. Brit. XIX. 273/2  				The mineral also often occurs in compact fibrous aggregates, the fibres having a divergent or radial arrangement (hence the name radiolite for one variety). 1993    A. M. Clark Hey's Mineral Index 		(ed. 3)	 583/2  				Radiolite,..a provisional name for the material later recognised as natrolite (of Klaproth). Named from its radiating habit. This entry has been updated (OED Third Edition, June 2008; most recently modified version published online March 2022). <  | 
	
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