Walter de Gruyter
Geochronometria
,  volume 48 ,  issue 1 ,  pages 197-204

Electron Spin Resonance (ESR) Signal Intensity of Quartz E1′ Centre and Its Potential Use in Fluvial Sediments Provenance Tracing

Chuan Yi Wei 1, 2
, 
Chun Ru Liu 1
, 
Gong-Ming Yin 1
, 
Wen Peng Li 1, 3
1
 
State Key Laboratory of Earthquake Dynamics , Institute of Geology, China Earthquake Administration , Beijing , China | 
2
 
3
 
Publication type: Journal Article
Publication date: 2021-01-01
Walter de Gruyter
scimago Q3
wos Q4
SJR: 0.326
CiteScore: 3.1
Impact factor: 0.9
ISSN: 17338387, 18971695
Earth and Planetary Sciences (miscellaneous)
Abstract

To assess if the heat-treated E 1′ centre in quartz is suitable for fluvial sediment provenance tracing, eight granitic samples from sediments and their source rocks with distinct geological ages and origins were collected for electron spin resonance (ESR) measurements. The results show that the maximum heat-treated E 1′ signal intensity of quartz in the fluvial sediments occurs upon heating at about 300°C, as previously observed in aeolian quartz. The heat-treated E 1′ signal intensity of quartz in sediment samples also shows significant correspondence to those of their source rocks as well as their formation age. We propose that the heat-treated E 1′ centre of sedimentary quartz, combined with other lithological discrimination parameters, could serve as an effective indicator for fluvial sediment provenance tracing.

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Wei C. Y. et al. Electron Spin Resonance (ESR) Signal Intensity of Quartz E1′ Centre and Its Potential Use in Fluvial Sediments Provenance Tracing // Geochronometria. 2021. Vol. 48. No. 1. pp. 197-204.
GOST all authors (up to 50) Copy
Wei C. Y., Liu C. R., Yin G., Li W. P. Electron Spin Resonance (ESR) Signal Intensity of Quartz E1′ Centre and Its Potential Use in Fluvial Sediments Provenance Tracing // Geochronometria. 2021. Vol. 48. No. 1. pp. 197-204.
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RIS Copy
TY - JOUR
DO - 10.2478/geochr-2020-0040
UR - https://doi.org/10.2478/geochr-2020-0040
TI - Electron Spin Resonance (ESR) Signal Intensity of Quartz E1′ Centre and Its Potential Use in Fluvial Sediments Provenance Tracing
T2 - Geochronometria
AU - Wei, Chuan Yi
AU - Liu, Chun Ru
AU - Yin, Gong-Ming
AU - Li, Wen Peng
PY - 2021
DA - 2021/01/01
PB - Walter de Gruyter
SP - 197-204
IS - 1
VL - 48
SN - 1733-8387
SN - 1897-1695
ER -
BibTex |
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BibTex (up to 50 authors) Copy
@article{2021_Wei,
author = {Chuan Yi Wei and Chun Ru Liu and Gong-Ming Yin and Wen Peng Li},
title = {Electron Spin Resonance (ESR) Signal Intensity of Quartz E1′ Centre and Its Potential Use in Fluvial Sediments Provenance Tracing},
journal = {Geochronometria},
year = {2021},
volume = {48},
publisher = {Walter de Gruyter},
month = {jan},
url = {https://doi.org/10.2478/geochr-2020-0040},
number = {1},
pages = {197--204},
doi = {10.2478/geochr-2020-0040}
}
MLA
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MLA Copy
Wei, Chuan Yi, et al. “Electron Spin Resonance (ESR) Signal Intensity of Quartz E1′ Centre and Its Potential Use in Fluvial Sediments Provenance Tracing.” Geochronometria, vol. 48, no. 1, Jan. 2021, pp. 197-204. https://doi.org/10.2478/geochr-2020-0040.