Acceso abierto

Characteristics of ESR signals and TLCLs of quartz included in various source rocks and sediments in Japan: A clue to sediment provenance

Geochronometria's Cover Image
Geochronometria
Special Issue Title: Proceedings of the 3rd Asia Pacific Conference on Luminescence and Electron Spin Resonance Dating Okayama, Japan, 2012

Cite

[1] Aitken MJ, 1985. Thermoluminesence dating. Academic Press. London, 359p. Search in Google Scholar

[2] Aitken MJ, 1998. An introduction to optical dating. Oxford Science Publications, 267p. Search in Google Scholar

[3] Feigl FJ, Fowler WB and Yip KL, 1974. Oxygen vacancy model for the E1’ centre in SiO2. Solid State Communications 14(3): 225–229, DOI 10.1016/0038-1098(74)90840-0. http://dx.doi.org/10.1016/0038-1098(74)90840-010.1016/0038-1098(74)90840-0Search in Google Scholar

[4] Ganzawa Y, Watanabe Y, Osanai F and Hashimoto T, 1997. TL colour images from quartzes of loess and tephra in China and Japan. Radiation Measurements 27(2): 383–388, DOI 10.1016/S1350-4487(96)00129-1. http://dx.doi.org/10.1016/S1350-4487(96)00129-110.1016/S1350-4487(96)00129-1Search in Google Scholar

[5] Hashimoto T, Koyanagi A, Yokosaka K, Hayashi Y and Sotobayashi T, 1986. Themoluminecence colour images from quartz of beach sands. Geochemical Journal 20(3): 111–118. http://dx.doi.org/10.2343/geochemj.20.11110.2343/geochemj.20.111Search in Google Scholar

[6] Hashimoto T, Katayama H, Sakaue H, Hase H, Arimura T and Ojima T, 1997. Dependence of some radiation-induced phenomena from natural quartz on hydroxyl-impurity contents. Radiation Measurements 27(2): 243–250, DOI 10.1016/S1350-4487(96)00115-1. http://dx.doi.org/10.1016/S1350-4487(96)00115-110.1016/S1350-4487(96)00115-1Search in Google Scholar

[7] Ikeya M, 1993. New Applications of Electron Spin Resonance, Dating, Dosimetry, and Microscopy. World Scientific, Singapore, 500p. 10.1142/1854Search in Google Scholar

[8] Duttinea M, Villeneuvea G, Bechtela F and Demazeaub G, 2002. Caractérisation par résonance paramagnétique électronique (RPE) de quartz naturels issus de différentes sources (Characterization by electron paramagnetic resonance (EPR) of natural quartz, problem of source differentiation). Comptes Rendus Geoscience 334(13): 949–955, DOI 10.1016/S1631-0713(02)01845-X. http://dx.doi.org/10.1016/S1631-0713(02)01845-X10.1016/S1631-0713(02)01845-XSearch in Google Scholar

[9] Murata K and M Norman, 1976. An index of crystallinity for quartz. American Journal of Science 276(9): 1120–1130, DOI 10.2475/ajs.276.9.1120. http://dx.doi.org/10.2475/ajs.276.9.112010.2475/ajs.276.9.1120Search in Google Scholar

[10] Nagashima K, Tada R, Tani A, Toyoda S, Sun Y, and Isozaki Y, 2007. Contribution of aeolian dust in Japan Sea sediments estimated from ESR signal intensity and crystallinity of quartz. Geochemistry, Geophysics, Geosystems 8(2), DOI 10.1029/2006GC001364. 10.1029/2006GC001364Search in Google Scholar

[11] Naruse T, Ono Y, Hirakawa K, Okashita M, and Ikeya M, 1997. Source areas of eolian dust quartz in East Asia: a tentative reconstruction of prevailing winds in isotope stage 2 using electron spin resonance. Geographical review of Japan 70A-1: 15–27. 10.4157/grj1984a.70.1_15Search in Google Scholar

[12] Ohta M, Asami S and Sakaguchi M, 1992. Luminescence and ESR Characteristics of Glaserite Crystals Doped with Europium Ion. Denki Kagaku oyobi Kogyo Butsuri Kagaku 60(7): 643–648. 10.5796/electrochemistry.60.643Search in Google Scholar

[13] Sawakuchi AO, Blair MW, DeWitt R, Faleiros FM, Hyppolito T and Guedes CCF, 2011. Thermal history versus sedimentary history: OSL sensitivity of quartz grains extracted from rocks and sediments. Quaternary Geochronology 6(2): 261–272, DOI 10.1016/j.quageo.2010.11.002. http://dx.doi.org/10.1016/j.quageo.2010.11.00210.1016/j.quageo.2010.11.002Search in Google Scholar

[14] Toyoda S and Hattori M, 2000. Formation and decay of the E1’ centre and of its precursor. Applied Radiation and Isotopes 52(5): 1351–1356, DOI 10.1016/S0969-8043(00)00094-4. http://dx.doi.org/10.1016/S0969-8043(00)00094-410.1016/S0969-8043(00)00094-4Search in Google Scholar

[15] Toyoda S and Naruse T, 2002. Eolian Dust from Asia Deserts to Japanese Island since the last Glacial Maximum: the Basis for the ESR Method. Japan Geomorphological union 23–5: 811–820. Search in Google Scholar

[16] Toyoda S and Falguères C, 2003. The method to represent the ESR intensity of the aluminium hole centre in quartz for the purpose of dating. Advances in ESR applications 20: 7–10. Search in Google Scholar

[17] Toyoda S, Voinchet P, Falguères C, Dolo JM and Laurent M, 2000. Bleaching of ESR signals by the sunlight: a laboratory experiment for establishing the ESR dating of sediments. Applied Radiation and Isotopes 52(5): 1357–1362, DOI 10.1016/S0969-8043(00)00095-6. http://dx.doi.org/10.1016/S0969-8043(00)00095-610.1016/S0969-8043(00)00095-6Search in Google Scholar

[18] Shimada A and Takada M, 2008. Characteristics of Electron Spin Resonance (ESR) signals in quartz from igneous rock samples: a clue to sediment provenance. Annual Reports of Graduate School of Humanities and Sciences 23: 187–195. Search in Google Scholar

[19] Yawata T, Takeuchi T and Hashimoto T, 2006. Dependence of luminescence sensitivity of quartz on α-β phase inversion berak temperatures. Radiation Measurements 41(7–8): 841–846, DOI 10.1016/j.radmeas.2006.05.008. 10.1016/j.radmeas.2006.05.008Search in Google Scholar

[20] Yokoyama Y, Falguères C and Quaegebeur JP, 1985. ESR dating of quartz from quaternary sediments: first attempt. Nuclear Tracks and Radiation Measurements 10(4–6): 921–928, DOI 10.1016/0735-245X (85)90109-7. 10.1016/0735-245X(85)90109-7Search in Google Scholar

eISSN:
1897-1695
Idioma:
Inglés
Calendario de la edición:
Volume Open
Temas de la revista:
Geosciences, other