STRUCTURAL PHASE TRANSITIONS IN NATROLITE AT HIGH PRESSURES

dc.contributor.authorBelitskiy I.A.
dc.contributor.authorFursenko B.A.
dc.contributor.authorKholedeyev O.V.
dc.contributor.authorGoryaynov S.V.
dc.date.accessioned2020-04-16T07:06:01Z
dc.date.available2020-04-16T07:06:01Z
dc.date.issued1987
dc.description.abstractData is presented on the behavior of natural natrolite Na 2Al 2Si 3O 10·2H 2O from the Kola Peninsula under hydrostatic pressures of up to 50 kbar at room temperature. We studied transparent colorless prismatic monocrystalline blocks measuring 100 to 300 μm on a side, bounded by the (110 and (1̄10) cleavage planes. The experiments were run in a high-pressure unit with diamond anvils [9], and the measurements were made by optical polarization microscopy, multichannel Raman microspectroscopy and X-ray diffraction. Experimental evidence indicates that the behavior of natrolite under pressure in penetrative and nonpenetrative media differed significantly. When natrolite was compressed in water, we found two reversible phase transitions: natrolite I → II at 7.5 kbar, and natrolite II → III at 12.5 kbar. The natrolite I → II structural transition under pressure is reflected in the Raman spectra obtained.
dc.identifierhttps://elibrary.ru/item.asp?id=31023794
dc.identifier.citationTRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1987, 297, 6, 148-152
dc.identifier.issn0891-5571
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/16867
dc.titleSTRUCTURAL PHASE TRANSITIONS IN NATROLITE AT HIGH PRESSURES
dc.typeСтатья

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