Standard
Composition of the gases from minerals of corundum-bearing rocks from the belomorian mobile belt (North Karelia, Russia). / Akimova, Ekaterina; Verchovsky, Alexander; Kozlov, Evgeniy; Lokhov, Kirill.
17TH INTERNATIONAL MULTIDISCIPLINARY SCIENTIFIC GEOCONFERENCE SGEM 2017: Albena, Bulgaria, 29 июня-05 июля 2017 г. Conference proceedings, GEOLOGY, MINERAL PROCESSING. Vol. 17, Issue 11 STEF92 Technology Ltd., 2017. p. 103-108 (International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM; Vol. 17, No. 11).
Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › peer-review
Harvard
Akimova, E, Verchovsky, A, Kozlov, E
& Lokhov, K 2017,
Composition of the gases from minerals of corundum-bearing rocks from the belomorian mobile belt (North Karelia, Russia). in
17TH INTERNATIONAL MULTIDISCIPLINARY SCIENTIFIC GEOCONFERENCE SGEM 2017: Albena, Bulgaria, 29 июня-05 июля 2017 г. Conference proceedings, GEOLOGY, MINERAL PROCESSING. vol. 17, Issue 11, International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM, no. 11, vol. 17, STEF92 Technology Ltd., pp. 103-108, 17th International Multidisciplinary Scientific Geoconference, SGEM 2017, Albena, Bulgaria,
29/06/17.
https://doi.org/10.5593/sgem2017/11/S01.013
APA
Akimova, E., Verchovsky, A., Kozlov, E.
, & Lokhov, K. (2017).
Composition of the gases from minerals of corundum-bearing rocks from the belomorian mobile belt (North Karelia, Russia). In
17TH INTERNATIONAL MULTIDISCIPLINARY SCIENTIFIC GEOCONFERENCE SGEM 2017: Albena, Bulgaria, 29 июня-05 июля 2017 г. Conference proceedings, GEOLOGY, MINERAL PROCESSING (Vol. 17, Issue 11, pp. 103-108). (International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM; Vol. 17, No. 11). STEF92 Technology Ltd..
https://doi.org/10.5593/sgem2017/11/S01.013
Vancouver
Akimova E, Verchovsky A, Kozlov E
, Lokhov K.
Composition of the gases from minerals of corundum-bearing rocks from the belomorian mobile belt (North Karelia, Russia). In 17TH INTERNATIONAL MULTIDISCIPLINARY SCIENTIFIC GEOCONFERENCE SGEM 2017: Albena, Bulgaria, 29 июня-05 июля 2017 г. Conference proceedings, GEOLOGY, MINERAL PROCESSING. Vol. 17, Issue 11. STEF92 Technology Ltd. 2017. p. 103-108. (International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM; 11).
https://doi.org/10.5593/sgem2017/11/S01.013
Author
Akimova, Ekaterina ; Verchovsky, Alexander ; Kozlov, Evgeniy
; Lokhov, Kirill. /
Composition of the gases from minerals of corundum-bearing rocks from the belomorian mobile belt (North Karelia, Russia). 17TH INTERNATIONAL MULTIDISCIPLINARY SCIENTIFIC GEOCONFERENCE SGEM 2017: Albena, Bulgaria, 29 июня-05 июля 2017 г. Conference proceedings, GEOLOGY, MINERAL PROCESSING. Vol. 17, Issue 11 STEF92 Technology Ltd., 2017. pp. 103-108 (International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM; 11).
BibTeX
@inproceedings{7d69f8b8d68c4c3899866f6102b2d1d6,
title = "Composition of the gases from minerals of corundum-bearing rocks from the belomorian mobile belt (North Karelia, Russia)",
abstract = "Isotopic composition of noble gases and other volatiles (CO2, N2) from minerals of corundum-bearing rocks with isotopically ultralight oxygen from Khitoostrov deposit have been investigated. The studies were conducted on Finesse mass-spectrometry system [1] using step heating in temperature range from 200ºС to 1400ºС. The following minerals were investigated: corundum, amphibole, garnet, staurolite. For the same samples, differential scanning calorimetry and thermogravimetry curves have been obtained. The first results of the studies show that the low-temperature (less than 400°C) release peaks of carbon dioxide and nitrogen probably represent a laboratory organic contamination. The middle-temperature release peaks (400-800ºC) are potentially consistent with decrepitation of fluid inclusions and diffusion of the gases from crystalline lattice of the minerals, and the high-temperature release peaks (900-1400ºC) possibly indicate the transformation of mineral structures such as amphibole and staurolite as a result of dehydration.",
keywords = "Corundum-bearing rocks, Noble gas, Thermal analysis",
author = "Ekaterina Akimova and Alexander Verchovsky and Evgeniy Kozlov and Kirill Lokhov",
year = "2017",
month = jan,
day = "1",
doi = "10.5593/sgem2017/11/S01.013",
language = "English",
isbn = " 978-619-7105-98-8",
volume = "17, Issue 11",
series = "International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM",
publisher = "STEF92 Technology Ltd.",
number = "11",
pages = "103--108",
booktitle = "17TH INTERNATIONAL MULTIDISCIPLINARY SCIENTIFIC GEOCONFERENCE SGEM 2017",
address = "Bulgaria",
note = "17th International Multidisciplinary Scientific Geoconference, SGEM 2017, SGEM 2017 ; Conference date: 29-06-2017 Through 05-07-2017",
}
RIS
TY - GEN
T1 - Composition of the gases from minerals of corundum-bearing rocks from the belomorian mobile belt (North Karelia, Russia)
AU - Akimova, Ekaterina
AU - Verchovsky, Alexander
AU - Kozlov, Evgeniy
AU - Lokhov, Kirill
PY - 2017/1/1
Y1 - 2017/1/1
N2 - Isotopic composition of noble gases and other volatiles (CO2, N2) from minerals of corundum-bearing rocks with isotopically ultralight oxygen from Khitoostrov deposit have been investigated. The studies were conducted on Finesse mass-spectrometry system [1] using step heating in temperature range from 200ºС to 1400ºС. The following minerals were investigated: corundum, amphibole, garnet, staurolite. For the same samples, differential scanning calorimetry and thermogravimetry curves have been obtained. The first results of the studies show that the low-temperature (less than 400°C) release peaks of carbon dioxide and nitrogen probably represent a laboratory organic contamination. The middle-temperature release peaks (400-800ºC) are potentially consistent with decrepitation of fluid inclusions and diffusion of the gases from crystalline lattice of the minerals, and the high-temperature release peaks (900-1400ºC) possibly indicate the transformation of mineral structures such as amphibole and staurolite as a result of dehydration.
AB - Isotopic composition of noble gases and other volatiles (CO2, N2) from minerals of corundum-bearing rocks with isotopically ultralight oxygen from Khitoostrov deposit have been investigated. The studies were conducted on Finesse mass-spectrometry system [1] using step heating in temperature range from 200ºС to 1400ºС. The following minerals were investigated: corundum, amphibole, garnet, staurolite. For the same samples, differential scanning calorimetry and thermogravimetry curves have been obtained. The first results of the studies show that the low-temperature (less than 400°C) release peaks of carbon dioxide and nitrogen probably represent a laboratory organic contamination. The middle-temperature release peaks (400-800ºC) are potentially consistent with decrepitation of fluid inclusions and diffusion of the gases from crystalline lattice of the minerals, and the high-temperature release peaks (900-1400ºC) possibly indicate the transformation of mineral structures such as amphibole and staurolite as a result of dehydration.
KW - Corundum-bearing rocks
KW - Noble gas
KW - Thermal analysis
UR - http://www.scopus.com/inward/record.url?scp=85032461336&partnerID=8YFLogxK
U2 - 10.5593/sgem2017/11/S01.013
DO - 10.5593/sgem2017/11/S01.013
M3 - Conference contribution
AN - SCOPUS:85032461336
SN - 978-619-7105-98-8
VL - 17, Issue 11
T3 - International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM
SP - 103
EP - 108
BT - 17TH INTERNATIONAL MULTIDISCIPLINARY SCIENTIFIC GEOCONFERENCE SGEM 2017
PB - STEF92 Technology Ltd.
T2 - 17th International Multidisciplinary Scientific Geoconference, SGEM 2017
Y2 - 29 June 2017 through 5 July 2017
ER -
