A study of K-feldspars from the Serres-Drama plutonic complex, Northern Greece
dc.creator | Theodorikas, S. | en |
dc.date.accessioned | 2015-11-23T10:49:48Z | |
dc.date.available | 2015-11-23T10:49:48Z | |
dc.date.issued | 1998 | |
dc.identifier.issn | 0028-3649 | |
dc.identifier.uri | http://hdl.handle.net/11615/33624 | |
dc.description.abstract | The 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.subject | ALKALI FELDSPARS | en |
dc.subject | Mineralogy | en |
dc.title | A study of K-feldspars from the Serres-Drama plutonic complex, Northern Greece | en |
dc.type | journalArticle | en |
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