Abstract
Quarzites retrieved from the Sopks-248 deposit and Belokamenka deposit, Antonovsk field cluster (Russia, West Siberia) were studied by the infrared spectroscopy method. The silicate thickness alteration rate was determined and the most crystalline quartzite variations were identified by defining the crystallinity index Ki according infrared absorption spectrum. To calculate "crystallinity index" the ratio of quintet peaks of 778 cm-1 as to peaks of 695 cm-1 were applied. It should be noted that the most crystalline quartzite variations are characterized by the relative value of crystallinity index.
| Original language | English |
|---|---|
| Article number | 012006 |
| Journal | IOP Conference Series: Earth and Environmental Science |
| Volume | 21 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 2014 |
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ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)
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Calculation of quarzite crystallinity index by infrared absorption spectrum. / Razva, O.; Anufrienkova, A.; Korovkin, M.; Ananieva, L.; Abramova, R.
In: IOP Conference Series: Earth and Environmental Science, Vol. 21, No. 1, 012006, 2014.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Calculation of quarzite crystallinity index by infrared absorption spectrum
AU - Razva, O.
AU - Anufrienkova, A.
AU - Korovkin, M.
AU - Ananieva, L.
AU - Abramova, R.
PY - 2014
Y1 - 2014
N2 - Quarzites retrieved from the Sopks-248 deposit and Belokamenka deposit, Antonovsk field cluster (Russia, West Siberia) were studied by the infrared spectroscopy method. The silicate thickness alteration rate was determined and the most crystalline quartzite variations were identified by defining the crystallinity index Ki according infrared absorption spectrum. To calculate "crystallinity index" the ratio of quintet peaks of 778 cm-1 as to peaks of 695 cm-1 were applied. It should be noted that the most crystalline quartzite variations are characterized by the relative value of crystallinity index.
AB - Quarzites retrieved from the Sopks-248 deposit and Belokamenka deposit, Antonovsk field cluster (Russia, West Siberia) were studied by the infrared spectroscopy method. The silicate thickness alteration rate was determined and the most crystalline quartzite variations were identified by defining the crystallinity index Ki according infrared absorption spectrum. To calculate "crystallinity index" the ratio of quintet peaks of 778 cm-1 as to peaks of 695 cm-1 were applied. It should be noted that the most crystalline quartzite variations are characterized by the relative value of crystallinity index.
UR - http://www.scopus.com/inward/record.url?scp=84906952775&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84906952775&partnerID=8YFLogxK
U2 - 10.1088/1755-1315/21/1/012006
DO - 10.1088/1755-1315/21/1/012006
M3 - Article
VL - 21
JO - IOP Conference Series: Earth and Environmental Science
JF - IOP Conference Series: Earth and Environmental Science
SN - 1755-1307
IS - 1
M1 - 012006
ER -