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pericline : ウィキペディア英語版
pericline
:''Pericline also refers to a doubly plunging anticline or syncline.''
Pericline is a form of albite exhibiting elongate prismatic crystals.〔(Mindat with location data )〕
Pericline twinning is a type of crystal twinning which show fine parallel twin laminae typically found in the alkali feldspars microcline.〔Hurlbut, Cornelius S.; Klein, Cornelis, 1985, ''Manual of Mineralogy'', p. 100, 20th ed., ISBN 0-471-80580-7 〕 The twinning results from a structural transformation between high temperature and low temperature forms.〔Tsatskis, I. and E.K.H. Salje (1996) ''Time evolution of pericline twin domains in alkali feldspars'', American Mineralogist, Volume 81, pages 800-810 (PDF )〕
==References==


抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「pericline」の詳細全文を読む



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