X-ray studies have established that as a result of the thermal impact on the quartz-pyrophyllite rocks of the Boynxaksa deposit, the decomposition of the pyrophyllite phase begins at temperatures above 600 °C. The formation of the mullite phase is fixed at 1200 °C. The phase of cristobalite appears at 1300 oC and begins to prevail over the content of quartz at 1400 °C.
| Mualliflar | R. V. Mkrtchyan |
|---|---|
| Jurnal | Kimyo va kimyo texnologiyasi |
| Nashriyot | Тошкент кимё-технология институти |
| ISSN | 1992-9498, 2181-1121 |
| Nashr sanasi | 2019-10-18 |
| Jild | 2018 |
| Son | 2 |
| Til | Ingliz |
| DOI | 10.70189/1992-9498.1019 |
| Indeksga qo‘shilgan | 2026-09-02 |
DOI: 10.70189/1992-9498.1019 · Maqolaning asl sahifasi
| APA | R. V. Mkrtchyan (2019). PHASE CHANGES OF QUARTZ-PYROPHYLLITE ROCK OF BOYNAKSAY DEPOSIT BY THERMAL INFLUENCE. Kimyo va kimyo texnologiyasi, 2018(2). https://doi.org/10.70189/1992-9498.1019 |
|---|---|
| GOST (OAK) | R. V. Mkrtchyan PHASE CHANGES OF QUARTZ-PYROPHYLLITE ROCK OF BOYNAKSAY DEPOSIT BY THERMAL INFLUENCE // Kimyo va kimyo texnologiyasi. – 2019. – T. 2018, № 2. – DOI: 10.70189/1992-9498.1019. |
| MLA | R. V. Mkrtchyan. “PHASE CHANGES OF QUARTZ-PYROPHYLLITE ROCK OF BOYNAKSAY DEPOSIT BY THERMAL INFLUENCE.” Kimyo va kimyo texnologiyasi, 2018(2), 2019. https://doi.org/10.70189/1992-9498.1019 |
| Chicago | R. V. Mkrtchyan. “PHASE CHANGES OF QUARTZ-PYROPHYLLITE ROCK OF BOYNAKSAY DEPOSIT BY THERMAL INFLUENCE.” Kimyo va kimyo texnologiyasi, 2018(2) (2019). https://doi.org/10.70189/1992-9498.1019 |
| Harvard | R. V. Mkrtchyan (2019) ‘PHASE CHANGES OF QUARTZ-PYROPHYLLITE ROCK OF BOYNAKSAY DEPOSIT BY THERMAL INFLUENCE’, Kimyo va kimyo texnologiyasi, 2018(2). https://doi.org/10.70189/1992-9498.1019 |
| BibTeX | @article{rvmkrtchyan2019,
title = {PHASE CHANGES OF QUARTZ-PYROPHYLLITE ROCK OF BOYNAKSAY DEPOSIT BY THERMAL INFLUENCE},
author = {R. V. Mkrtchyan},
journal = {Kimyo va kimyo texnologiyasi},
year = {2019},
volume = {2018},
number = {2},
doi = {10.70189/1992-9498.1019},
url = {https://doi.org/10.70189/1992-9498.1019}
} |
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