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Formation Parameters of High-Pressure Minerals in the Dhofar 717 and 864 Chondrite Meteorites. / Litasov, K. D.; Badyukov, D. D.; Pokhilenko, N. P.

в: Doklady Earth Sciences, Том 485, № 1, 01.03.2019, стр. 327-330.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Litasov, KD, Badyukov, DD & Pokhilenko, NP 2019, 'Formation Parameters of High-Pressure Minerals in the Dhofar 717 and 864 Chondrite Meteorites', Doklady Earth Sciences, Том. 485, № 1, стр. 327-330. https://doi.org/10.1134/S1028334X19030322

APA

Litasov, K. D., Badyukov, D. D., & Pokhilenko, N. P. (2019). Formation Parameters of High-Pressure Minerals in the Dhofar 717 and 864 Chondrite Meteorites. Doklady Earth Sciences, 485(1), 327-330. https://doi.org/10.1134/S1028334X19030322

Vancouver

Litasov KD, Badyukov DD, Pokhilenko NP. Formation Parameters of High-Pressure Minerals in the Dhofar 717 and 864 Chondrite Meteorites. Doklady Earth Sciences. 2019 март 1;485(1):327-330. doi: 10.1134/S1028334X19030322

Author

Litasov, K. D. ; Badyukov, D. D. ; Pokhilenko, N. P. / Formation Parameters of High-Pressure Minerals in the Dhofar 717 and 864 Chondrite Meteorites. в: Doklady Earth Sciences. 2019 ; Том 485, № 1. стр. 327-330.

BibTeX

@article{6a7c8937e2de4e4f930e67fd8d8b8a91,
title = "Formation Parameters of High-Pressure Minerals in the Dhofar 717 and 864 Chondrite Meteorites",
abstract = "This paper presents the results of a Raman spectroscopic study of shock melt veins in L6 chondritic meteorites Dhofar 717 and 864, and conclusions about the P–T parameters recorded in these meteorites after the impact event. The primary minerals of the host chondrite include olivine, orthopyroxene, clinopyroxene, plagioclase, chromite, phosphates, troilite, and kamasite. Shock melt veins up to 1 cm thick contain fragments of the high-pressure minerals ringwoodite, wadsleyite, majorite, akimotoite, jadeite, lingunite, and tuite and quenched melt consisting of majorite, ringwoodite, troilite, and kamasite. The mineral associations of the Dhofar 717 and 864 chondrites indicate high peak PT parameters of the impact in the region of stability of majorite (>20 GPa and >2500 K) and bridgmanite (>25 GPa and >2500 K). The presence of lingunite also directly indicates a peak pressure in the area of stability of the bridgmanite.",
author = "Litasov, {K. D.} and Badyukov, {D. D.} and Pokhilenko, {N. P.}",
year = "2019",
month = mar,
day = "1",
doi = "10.1134/S1028334X19030322",
language = "English",
volume = "485",
pages = "327--330",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Formation Parameters of High-Pressure Minerals in the Dhofar 717 and 864 Chondrite Meteorites

AU - Litasov, K. D.

AU - Badyukov, D. D.

AU - Pokhilenko, N. P.

PY - 2019/3/1

Y1 - 2019/3/1

N2 - This paper presents the results of a Raman spectroscopic study of shock melt veins in L6 chondritic meteorites Dhofar 717 and 864, and conclusions about the P–T parameters recorded in these meteorites after the impact event. The primary minerals of the host chondrite include olivine, orthopyroxene, clinopyroxene, plagioclase, chromite, phosphates, troilite, and kamasite. Shock melt veins up to 1 cm thick contain fragments of the high-pressure minerals ringwoodite, wadsleyite, majorite, akimotoite, jadeite, lingunite, and tuite and quenched melt consisting of majorite, ringwoodite, troilite, and kamasite. The mineral associations of the Dhofar 717 and 864 chondrites indicate high peak PT parameters of the impact in the region of stability of majorite (>20 GPa and >2500 K) and bridgmanite (>25 GPa and >2500 K). The presence of lingunite also directly indicates a peak pressure in the area of stability of the bridgmanite.

AB - This paper presents the results of a Raman spectroscopic study of shock melt veins in L6 chondritic meteorites Dhofar 717 and 864, and conclusions about the P–T parameters recorded in these meteorites after the impact event. The primary minerals of the host chondrite include olivine, orthopyroxene, clinopyroxene, plagioclase, chromite, phosphates, troilite, and kamasite. Shock melt veins up to 1 cm thick contain fragments of the high-pressure minerals ringwoodite, wadsleyite, majorite, akimotoite, jadeite, lingunite, and tuite and quenched melt consisting of majorite, ringwoodite, troilite, and kamasite. The mineral associations of the Dhofar 717 and 864 chondrites indicate high peak PT parameters of the impact in the region of stability of majorite (>20 GPa and >2500 K) and bridgmanite (>25 GPa and >2500 K). The presence of lingunite also directly indicates a peak pressure in the area of stability of the bridgmanite.

UR - http://www.scopus.com/inward/record.url?scp=85066476684&partnerID=8YFLogxK

U2 - 10.1134/S1028334X19030322

DO - 10.1134/S1028334X19030322

M3 - Article

AN - SCOPUS:85066476684

VL - 485

SP - 327

EP - 330

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 25754680