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Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/13359
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dc.contributor.advisorBurley, B.J.en_US
dc.contributor.authorAnderson, Ascroft Mackenzie Peteren_US
dc.date.accessioned2014-06-18T17:03:44Z-
dc.date.available2014-06-18T17:03:44Z-
dc.date.created2013-09-23en_US
dc.date.issued1968-05en_US
dc.identifier.otheropendissertations/8181en_US
dc.identifier.other9350en_US
dc.identifier.other4613651en_US
dc.identifier.urihttp://hdl.handle.net/11375/13359-
dc.description.abstract<p>A study was made of the phase relationships in the system NaAlSiO<sub>4</sub>-NaOH-H<sub>2</sub>O, at 15,000 p.s.i. and at 450°C, 520°C, 600°C and 700°C. The following phases were found and characterised: hydroxyl varieties of nosean, sodalite and cancrinite, with formulae approximating to 3NaAlSiO<sub>4</sub>.NaOH.xH<sub>2</sub>O, 1x1.5, sodic nepheline and phase X, apparently a previously unreported phase, with composition approaching Na<sub>4</sub>Al<sub>2</sub>Si<sub>2</sub>O<sub>9</sub>. Approximate phase diagrams were deduced for the four temperatures.</p>en_US
dc.subjectGeologyen_US
dc.subjectGeologyen_US
dc.subjectGeologyen_US
dc.titlePhase Relations of the Hydroxyl Felspathoids in the System NaAlSiO4-NaOH-H20en_US
dc.typethesisen_US
dc.contributor.departmentGeologyen_US
dc.description.degreeDoctor of Philosophy (PhD)en_US
Appears in Collections:Open Access Dissertations and Theses

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