Pregled bibliografske jedinice broj: 573428
A comparative study of the luminescence characteristics of polymineral fine grains and coarse grained K-, Na- rich feldspars
A comparative study of the luminescence characteristics of polymineral fine grains and coarse grained K-, Na- rich feldspars // Radiation measurements, 47 (2012), 9; 903-908 doi:10.1016/j.radmeas.2012.02.017 (međunarodna recenzija, članak, znanstveni)
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Naslov
A comparative study of the luminescence characteristics of polymineral fine grains and coarse grained K-, Na- rich feldspars
(A comparative study of the luminescence characteristics of polymineral fine grains and coarse grained K- and Na- rich feldspars)
Autori
Tsukamoto, Sumiko ; Jain, Mayank ; Murray, Andrew S. ; Thiel, Christine ; Schmidt, Esther D. ; Wacha, Lara ; Dohrmann, Reiner ; Frechen, Manfred
Izvornik
Radiation measurements (1350-4487) 47
(2012), 9;
903-908
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
feldspar; polymineral; IRSL; post-IR IRSL; thermal stability; time-resolved IRSL
Sažetak
The IRSL and post-IR IRSL (pIRIR) signal characteristics of polymineral fine grains are investigated and compared with those of K- and Na- feldspar extracts. TL signal loss after IR and pIRIR stimulations occur mainly at around 320°C for polymineral and Na-feldspar samples and around 410°C for K-feldspar samples, when a preheat temperature of 250°C for 60s is used. After preheating to a higher temperature (320°C for 60s), all samples show a TL reduction around 410°C in the blue detection window. Pulse annealing experiments for IRSL and pIRIR signals for preheats between 320°C and 500°C indicate that the signal stabilities are similar among the different feldspar types, when a higher preheat temperature (> 320°C) is used. Thermal activation energies for IRSL and pIRIR signals is the largest in K- feldspar and the smallest in polymineral fine grains in both blue and UV detection windows for both fast time-resolved (TR) and continuous wave (CW) signals. These results suggest that IRSL and pIRIR signals in polymineral fine grains originate mainly from Na-feldspar grains ; these signals are less thermally stable than those from K-feldspar, but a more stable signal (presumably from K- feldspar grains) can be obtained by using a higher preheat temperature.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
181-1811096-1093 - Osnovna geološka karta Republike Hrvatske 1:50.000 (Belak, Mirko, MZOS ) ( CroRIS)
Ustanove:
Hrvatski geološki institut
Profili:
Lara Wacha
(autor)
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus