应用石英释光灵敏度溯源的研究现状和展望

吕同艳, 龚志军, 薛蕾. 应用石英释光灵敏度溯源的研究现状和展望[J]. 地质通报, 2016, 35(8): 1324-1331.
引用本文: 吕同艳, 龚志军, 薛蕾. 应用石英释光灵敏度溯源的研究现状和展望[J]. 地质通报, 2016, 35(8): 1324-1331.
LÜ Tongyan, GONG Zhijun, XUE Lei. Research on provenance using luminescence sensitivity of quartz grains: Progress and prospect[J]. Geological Bulletin of China, 2016, 35(8): 1324-1331.
Citation: LÜ Tongyan, GONG Zhijun, XUE Lei. Research on provenance using luminescence sensitivity of quartz grains: Progress and prospect[J]. Geological Bulletin of China, 2016, 35(8): 1324-1331.

应用石英释光灵敏度溯源的研究现状和展望

Research on provenance using luminescence sensitivity of quartz grains: Progress and prospect

  • 应用石英释光灵敏度进行物源研究是释光技术发展的新方向。回顾了石英释光灵敏度在测年研究中的发展现状,对其产生的机制、实验中的影响因素及其在测年中对灵敏度的监测、矫正等进行了介绍,详细介绍了空间尺度上不同沉积物(冰碛物、风成沉积物、水成沉积物)石英释光灵敏度的差异和时间序列上风成沉积物释光灵敏度的变化特征。据现有的研究成果分析,沉积历史和母岩来源对沉积物中石英的释光灵敏度的高低有重要的影响,因此可用它来追溯石英的物源。探讨该技术在物源研究领域存在的问题,对其发展前景进行了展望。
  • 加载中
  • [1]

    孙有斌,安芷生.风尘堆积物中石英颗粒表面微结构特征及其沉积学指示[J].沉积学报,2000,18(4):506-509.

    [2]

    黄求获,徐文强.我国不同海区沉积物石英颗粒表面的微结构[J].海洋科学,1997,21(2):43-47.

    [3]

    李珍,张家武.西宁黄土石英颗粒表面结构与黄土物质来源探讨[J].沉积学报,1999,17(2):221-225.

    [4]

    乔淑卿,杨作升.石英物源示源研究进展[J].海洋科学进展,2006,24(2):266-274.

    [5]

    侯圣山,杨石岭,丁仲礼.风成沉积物4~16μm石英氧同位素记录及其物质来源意义[J].中国科学(D辑),2003,33(6):535-542.

    [6]

    Rink W J.Electron spin resonance (ESR) dating and ESR applications in Quaternary science and archaeometry[J].Radiation Measurements,1997,27(5/6):975-1025.

    [7]

    业渝光,和杰,刁少波.沉积物中石英的ESR测年研究[J].核技术,1993,16(4):222-224.

    [8]

    张绍平,顿铁军.阴极发光显微镜在岩矿鉴定方面的应用[J].西安地质学院学报,1989,11(1):40-49.

    [9]

    Huntley D J,Godfrey-Smith D I,Thewalt M L W.Optical dating of sediments[J].Nature,1985,313(5998):105-107.

    [10]

    Aitken M J.ThermoluminescenceDating[M].Academic Press,1985:1-359.

    [11]

    Aitken M J.An Introduction to Optical Dating[M].Oxford University Press,1998:1-263.

    [12]

    Wintle A G,Catt J A.Thermoluminescence dating of soils developed in late devensian loess at pegwell bay,Kent[J].Journal of Soil Science,1985,36(2):293-298.

    [13]

    Wintle A G.A review of current research on TL dating of loess[J].Quaternary Science Reviews,1990,9(4):385-397.

    [14]

    Murray A S,Wintle A G.Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol[J].Radiation Measurements,2000,32(1):57-73.

    [15]

    Derbyshire E.Aeolian sediments in the Quaternary record:An introduction[J].Quaternary Science Reviews,1995,14(7/8):641-643.

    [16]

    Chithambo M L,Preusser F,Ramseyer K,et al.Time-resolved luminescence of low sensitivity quartz from crystalline rocks[J].Radiation Measurements,2007,42(2):205-212.

    [17]

    Lai Z P,Wintle A G.Locating the boundary between the Pleistocene and the Holocene in Chinese loess using luminescence[J].Holocene,2006,16(6):893-899.

    [18]

    Li S H,Chen Y Y,Li B,et al.OSL dating of sediments from deserts in northern China[J].Quaternary Geochronology,2007,2:23-28.

    [19]

    Zheng C X,Zhou L P,Qin J T.Difference in luminescence sensitivity of coarse-grained quartz from deserts of northern China[J].Radiation Measurements,2009,44(5):534-537.

    [20]

    Lü T Y,Sun J M.Luminescence sensitivities of quartz grains from eolian deposits in northern China and their implications for provenance[J].Quaternary Research,2011,76:181-189.

    [21]

    郑辰鑫,周力平.石英释光信号作为粉尘物源示踪手段的再研究[J].第四纪研究,2012,32(5):1036-1045.

    [22]

    Wintle A G,Murray A S.Luminescence sensitivity changes in quartz[J].Radiation Measurements,1999,30(1):107-118.

    [23]

    李盛华.光释光信号灵敏度变化的模式,验证和推论[J].核技术,1995,18(8):458-462.

    [24]

    Aitken M J,Smith B W.Optical dating-recuperation after bleaching[J].Quaternary Science Reviews,1988,7:387-393.

    [25]

    Bøtter-Jensen L,Duller G A T.A new system for measuring optically stimulated luminescence from quartz samples[J].International Journal of Radiation Apllications&Instrumentation.Part D.Nuclear Tracks&Radiation Measurements,1992,20(4):549-553.

    [26]

    Huntley D J,Godfreysmith D I,Haskell E H.Light-induced emission-spectra from some quartz and feldspars[J].Nuclear Tracks&Radiation Measurements,1991,18(1):127-131.

    [27]

    Stoneham D,Stokes S.An investigation of the relationship between the 110℃ TL peak and optically stimulated luminescence in sedimentary quartz[J].Nuclear Tracks&Radiation Measurements,1991,18(1/2):119-123.

    [28]

    Wintle A G,Murray A S.The relationship between quartz thermoluminescence,photo-transferred thermoluminescence,and optically stimulated luminescence[J].Radiation Measurements,1997,27(4):611-624.

    [29]

    Li S H.Luminescence sensitivity changes of quartz by bleaching,annealing and UV exposure[J].Radiation Effects and Defects in Solids,2002,157(3):357-364.

    [30]

    Murray A S,Rorberts R G.Measurement of the equivalent dose in quartz using a regenerative-dose single-aliquot protocol[J].Radiation Measurements,1998,29(5):503-515.

    [31]

    Zimmerman J.The radiation-induced increase of the 100℃ thermoluminescence sensitivity of fired quartz[J].Journal of Physics C:Solid State Physics,1971,4:3265-3275.

    [32]

    Bøtter-Jensen L,Agersnap L N,Mejdahl V,et al.Luminescence sensitivity changes in quartz as a result of annealing[J].Radiation Measurements,1995,24:535-541.

    [33]

    李虎侯.用石英110℃热释光峰灵敏度增高法测定年龄[J].核电子学与探测技术,1984,4(1):11-18.

    [34]

    尹功明,李盛华.石英的热释光前剂量特征及其在地学上的初步应用[J].地震地质,2000,12,22(增刊):37-41

    [35]

    王晓聆,张慧军,孙淼等.温度对细粒石英前剂量热释光响应的影响[J].中国医学物理学杂志,1998,15(2):116-117.

    [36]

    Roberts H M,Wintle A G.Luminescence sensitivity changes of polymineral fine grains during IRSL and[post-IR]OSL measurements[J].Radiation Measurements,2003,37(6):661-671.

    [37]

    Wintle A G,Murray A S.Towards the development of a preheat procedure for OSL dating of quartz[J].Radiation Measurements,1998,29(1):81-94.

    [38]

    Murray A S,Mejdahl V.Comparison of regenerative-dose singlealiquot and multiple-aliquot (SARA) protocols using heated quartz from archaeological sites[J].Quaternary science reviews,1999,18(2):223-229.

    [39]

    Murray A S,Wintle A G.The single aliquot regenerative dose protocol:potential for improvements in reliability[J].Radiation Measurements,2003,37(4):377-381.

    [40]

    Lu Y C,Wang X L,Wintle A G.A new OSL chronology for dust accumulation in the last 130,000yr for the Chinese Loess Plateau[J].Quaternary Research,2007,67(1):152-160.

    [41]

    Murray A S,Roberts R G,WintleA G.Equivalent dose measurement using a single aliquot of quartz[J].Radiation Measurements,1997,27(2):171-184.

    [42]

    Singhvi A K,Stokes S C,Chauhan N,et al.Changes in natural OSL sensitivity during single aliquot regeneration procedure and their implications for equivalent dose determination[J].Geochronometria,2011,38(3):231-241.

    [43]

    Rhodes E J.Quartz single grain OSL sensitivity distributions:Implications for multiple grain single aliquot dating[J].Geochronometria,2007,26(1):19-29.

    [44]

    Pietsch T J,Olleya J M,Nanson GC.Fluvial transport as a natural luminescence sensitiser of quartz[J].Quaternary Geochronology,2008,3(4):365-376.

    [45]

    Tsukamoto S,Nagashima K,Murray A S,et al.Variations in OSL components from quartz from Japan sea sediments and the possibility of reconstructing provenance[J].Quaternary International,2011,234(1):182-189.

    [46]

    Duller G A T.Single grain optical dating of glacigenicdeposits[J].Quaternary Geochronology,2006,1(4):296-304.

    [47]

    Fuchs M,Owen L A.Luminescence dating of glacial and associated sediments:review,recommendations and future directions[J].Boreas,2008,37(4):636-659.

    [48]

    Rhodes E J,Pownall L.Zeroing of the OSL signal in quartz from young glaciofluvialsediments[J].Radiation Measurements,1994,23(2):581-585.

    [49]

    RhodesE J,Bailey R M.The effect of thermal transfer on the zeroing of the luminescence of quartz from recent glaciofluvialsediments[J].Quaternary Science Reviews,1997,16(3):291-298.

    [50]

    Rhodes E J.Observations of thermal transfer OSL signals in glacigenicquartz[J].Radiation Measurements,2000,32(5):595-602.

    [51]

    Richards B.Luminescence dating of Quaternary sediments in the Himalaya and High Asia:a practical guide to its use and limitations for constraining the timing of glaciation[J].Quaternary International,2000,65(99):49-61.

    [52]

    Richthofen B F.Ⅱ-On the Mode of Origin of the Loess[J].Geological Magazine (Decade Ⅱ),1882,9(7):293-305.

    [53]

    Lukas S,Spencer J Q G,Robinson R A J,et al.Problems associated with luminescence dating of Late Quaternary glacial sediments in the NW Scottish Highlands[J].Quaternary Geochronology,2007,2(1):243-248.

    [54]

    Thrasher I M,Mauz B,Chiverrell R C,et al.Luminescence dating of glaciofluvial deposits:A review[J].Earth-Science Reviews,2009,97(1):133-146.

    [55]

    Sawakuchi A O,Blair M W,DeWitt R,et al.Thermal history versus sedimentary history:OSL sensitivity of quartz grains extracted from rocks and sediments[J].Quaternary Geochronology,2011,6(2):261-272.

    [56]

    Sawakuchi A O,Dewitt R,Blair M W,et al.Quartz OSL sensitivity as a proxy for storm activity on the southern Brazilian coast during the Late Holocene[J].Quaternary Geochronology,2012,13(6):92-102.

    [57]

    Zular A,Sawakuchi A O,Guedes C C F,et al.Attaining provenance proxies from OSL and TL sensitivities:Coupling with grain size and heavy minerals data from southern Brazilian coastal sediments[J].Radiation Measurements,2015,81:39-45.

    [58]

    Lü T Y,Sun J M,Li S H,et al.Vertical variations of luminescence sensitivity of quartz grains from loess/paleosol of Luochuan section in the central Chinese loess plateau since the last interglacial[J].Quaternary Geochronology,2014,22(3):107-115.

    [59]

    Wintle A G,Murray A S.A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols[J].Radiation Measurements,2006,41(4):369-391.

    [60]

    McKeever S W S,BotterJensen L,Larsen N A,et al.Optically stimulated luminescence sensitivity changes in quartz due to repeated use in single aliquot readout:Experiments and computer simulation[J].Radiation Protection Dosimetry,1996,65:49-54.

    [61]

    Moska P,Murray A S.Stability of the quartz fast-component in insensitive samples[J].Radiation Measurements,2006,41(7):878-885.

    [62]

    Koul D K,Chougaonkar M P.The pre-dose phenomenon in the OSL signal of quartz[J].Radiation Measurements,2007,42(8):1265-1272.

    [63]

    Preusser F,Chithambo M L,Gotte T,et al.Quartz as a natural luminescence dosimeter[J].Earth-Science Reviews,2009,97(1):184-214.

    [64]

    Preusser F,Ramseyer K,Schluchter C.Characterisation of low OSL intensity quartz from the New Zealand Alps[J].Radiation Measurements,2006,41(7/8):871-877.

    [65]

    Fitzsimmons K E,Rhodes E J,Barrows TT.OSL dating of southeast Australian quartz:A preliminary assessment of luminescence characteristics and behavior[J].Quaternary Geochronology,2010,5:91-95.

    [66]

    Dennen W H,Blackburn W H,Quesada A.Aluminum in quartz as a geothermometer[J].Contribution to Mineralogy and Petrology,1970,27(4):332-342.

    [67]

    Wark D A,Watson E B.TitaniQ:a titanium-in-quartz geothermometer[J].Contribution to Mineralogy and Petrology,2006,152(6):743-754.

    [68]

    Fitzsimmons K E.An assessment of the luminescence sensitivity of Australian quartz with respect to sediment history[J].Geochronometria,2011,38(3):199-208.

  • 加载中
计量
  • 文章访问数:  1356
  • PDF下载数:  63
  • 施引文献:  0
出版历程
收稿日期:  2015-12-11
修回日期:  2016-06-03
刊出日期:  2016-08-15

目录