TEMPERATURE-INDUCED P21/c TO C2/c PHASE TRANSITION IN PARTIALLY AMORPHOUS (METAMICT) TITANITE REVEALED BY RAMAN SPECTROSCOPY-Reference-Cited by-同舟云学术

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TEMPERATURE-INDUCED P21/c TO C2/c PHASE TRANSITION IN PARTIALLY AMORPHOUS (METAMICT) TITANITE REVEALED BY RAMAN SPECTROSCOPY

Published:2014-02-01 Issue:1 Volume:52 Page:91-100
ISSN:0008-4476
Container-title:The Canadian Mineralogist
language:en
Short-container-title:The Canadian Mineralogist

Author:

Beirau T.,Mihailova B.,Malcherek T.,Paulmann C.,Bismayer U.,Groat L. A.

Publisher

Mineralogical Association of Canada

Subject

Geochemistry and Petrology

Cited by 13 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Impact of actinide-induced crystal defects on REE-bearing titanite reactivity;Minerals Engineering;2022-03

2. Matrix effects and improved calibration procedures for SIMS titanite U Pb dating;Chemical Geology;2022-03

3. Temperature-versus compositional-induced structural deformations of gadolinite group minerals with various Be/B ratio;Journal of Solid State Chemistry;2021-07

4. Analysis of temperature‐dependent Raman spectra of minerals: Statistical approaches;Journal of Raman Spectroscopy;2020-02-11

5. Annealing of metamict gadolinite-(Y): X-ray diffraction, Raman, IR, and Mössbauer spectroscopy;Zeitschrift für Kristallographie - Crystalline Materials;2019-06-13

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