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dc.creatorTheodorikas, S.en
dc.date.accessioned2015-11-23T10:49:48Z
dc.date.available2015-11-23T10:49:48Z
dc.date.issued1998
dc.identifier.issn0028-3649
dc.identifier.urihttp://hdl.handle.net/11615/33624
dc.description.abstractThe variation in the structural state of potassium feldspars from the Serres-Drama plutonic complex, Northern Greece, from X-ray diffraction study is discussed. Monoclinic potassium feldspars occur in monzonitic rocks, which may have cooled with a much lower volatile content, whilst triclinic potassium feldspars occur in quartz monzonite, granodiorite and granite which probably cooled in the presence of a greater volatile content.en
dc.source.uri<Go to ISI>://WOS:000075378100001
dc.subjectALKALI FELDSPARSen
dc.subjectMineralogyen
dc.titleA study of K-feldspars from the Serres-Drama plutonic complex, Northern Greeceen
dc.typejournalArticleen


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