陆地和海洋环境演变研究中的释光测年进展

龚革联

陆地和海洋环境演变研究中的释光测年进展

龚革联

中国科学院广州地球化学研究所, 广州 510640

基金项目:

中国科学院边缘海地质重点实验室开放基金(MSGLCAS06-2)

详细信息

作者简介:
龚革联(1967-),男,高级工程师,博士生,从事释光年代学方面的研究工作,E-mail:gg11118@yahoo.com.cn

中图分类号: P597.3
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出版历程
- 收稿日期: 2005-10-23
- 修回日期: 2006-01-08

LUMINESCENCE DATING FOR ENVIRONMENTAL EVOLUTION STUDY IN TERRESTRIAL LAND,DEEP SEA AND COASTAL BELTS: A REVIEW

GONG Ge-lian

Guangzhou Institute of Geochemistry, CAS, Guangzhou 510064, China

摘要

摘要: 晚全新世以来所发生的特征环境事件的年龄测定,由于研究地区复杂及独特的地质条件,能够充分适用的测年方法有限,而释光测年方法(包括热释光和光释光方法)独有的揭示砂粒级无机成分末次曝光年龄的特点,正好适合于复杂的海岸带沉积环境,并且没有或者较少受到宇宙成因核素年代学分析方法中核素污染等干扰因素的影响。评述了释光测年方法的进展情况,并通过国内外在陆地、海洋和海陆带环境演变响应研究中几个成功运用释光测年方法的案例,分析了这种放射性测年方法的特点,并指出今后释光年代学方法研究的方向。
- 热释光 /
- 光释光 /
- 海陆交互带 /
- 环境演变响应
Abstract: Due to the complicated geological situation in coastal belts,very limited methods have ever been used for environmental study dealing with these zones,in particular the evidence of age concerning the typical environmental events within the Holocene period.Young ages mean their correlation with human activities,and the limitations of radionuclide dating methods,e.g.,¹⁰Be,radiocarbon and uranium/thorium,are normally used for coastal study.In contrast,luminescence dating method(both thermoluminescence and optical stimulated luminescence)can be successfully used for coastal belt study due to its exclusive feature of exploring age information of inorganic sand-size samples,whilst it is free of contamination resulting from radionuclide completely or partially.This paper discusses several cases and analyse the features of application of luminescence dating methods to studying environmental evolution in terrestrial land,deep sea and coastal belts as well as the future research work in this regard.
- thermoluminescence /
- optical stimulated luminescence /
- coastal belts /
- environmental evolution response

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参考文献(34)

[1]	Smith M A,Prescott J R,Head M J.Comparision of ¹⁴C and luminescence chronologies at Puritjarra Rock shelter,Central Australia[J].Quaternary Science Review,1997,16:299-320.
[2]	Prescott J R,Robertson G B.Sediment dating by luminescence:a review[J].Radiation Measurements,1997,27(5/6):893-922.
[3]	Madsen A T,Murray A S,Andersen T J,et al.Optically stimulated luminescence dating of young estuarine sediments:a comparison with ²¹⁰Pb and ¹³⁷Cs dating[J].Marine Geology,2005,214:251-268.
[4]	Murray A S,Olley J M.Precision and accuracy in the optically stimulated luminescence dating of sedimentary quartz:a status review[J].Geochronometria,2002,21:1-16.
[5]	Fattahi M.Studies on red thermoluminescence and infrared stimulated red luminescence[D].Unpublished D.Phil.thesis,Oxford University,Oxford,2001.
[6]	Scholefield R B,Prescott J R.The red thermoluminescence of quartz:3-D spectral measurements[J].Radiation Measurements,1999,30:83-95.
[7]	龚革联,刘顺生.长石矿物的三维热释光谱图初步研究[J].矿物岩石地球化学通报,2002,21:117-120.[GONG Ge-lian,LIU Shun-sheng.Preliminary study of characteristics of thermoluminescent spectra of feldspar[J].Bulletin of Mineralogy,Petrology and Geochemistry,2002 ,21(2):117-120.]
[8]	Scholefield R B,Prescott J R.The red thermoluminescence of quartz:3-D spectral measurements[J].Radiation Measurements,1999,30:83-95.
[9]	Pilleyre T,Montret M,Fain J,et al.Attempts at dating ancient volcanoes using the red TL of quartz[J].Quaternary Science Reviews,1992,11:13-17.
[10]	Fattahi M,Stokes S.Extending the time range of luminescence dating using red TL (RTL) from volcanic quartz[J].Radiation Measurements,2000,32:479-485.
[11]	Murray A S.Developments in optically stimulated luminescence and photo transferred thermoluminescence dating of young sediments:Application to 200 years sequences of flood sediments[J].Geochimica et Cosmochimica Acta,1996,60(4):565-576.
[12]	Bailey S D,Wintle A G,Duller G A T,et al.Sand deposition during the last millennium at Aberraw,Anglesey,North Wales as determined by OSL dating of quartz[J].Quat.Geochronol.(Quat.Sci.Rev.),2001,20:701-704.
[13]	Murray A S,Wintle A G.The single aliquot regenerative dose protocol:potential for improvements in reliability[J].Radiation Measurements,2003,37:377-381.
[14]	Wallinga J,Murray A S,Duller G A T,et al.Testing optically stimulated luminescence dating of sand-sized quartz and feldspar from fluvial deposits[J].Earth and Planetary Science Letters,2001,193:617-630.
[15]	McCoy D G,Prescott J R,Nation R J.Some aspects of single grain luminescence dating[J].Radiation Measurements,2000,32:859-864.
[16]	Bulur E,Bøtter-Jensen L,Murray A S.Optically stimulated luminescence from quartz measured using the linear modulation technique[J].Radiation Measurements,2000,32:407-411.
[17]	Steffen Greilich,Ulrich A Glasmacher,Günther A Wagner.Spatially resolved detection of luminescence:a unique tool for archaeochronometry[J].Naturwissenschaften,2002,89:371-375.
[18]	Ohn L Lawless,Lam S K,Lo D.Nondestructive in situ thermoluminescence using CO₂ laser heating[J].Optics Express,2002,10(6):291-296.
[19]	李虎侯. 选频光释光——一种新的年龄测定技术[J].自然科学进展,2002,12(3):333-336. [LI Hu-hou.Selected frequency optical stimulated luminescence-A new dating technique[J].Nature Science Progress,2002,12(3):333-336.]
[20]	Stephen Stokes,David S G,Thomas Richard Washinton.Multiple episodes of aridity in southern Africa since the last interglacial period[J].Nature,1997,388:154-158.
[21]	Fuchs M,Lang A,Wagner G A.The history of Holocene soil erosion in the Phlious Basin,NE Peloponnese,Greece,based on optical dating[J].The Holocene,2004,14(3):334-345.
[22]	Stokes S,Ingram S,Aitken M J,et al.Alternative chronologies for late Quaternary(Last Interglacial Holocene) deep sea sediment via optical dating of silt-size quartz[J].Quaternary Science Reviews,2003, 22:925-941.
[23]	Olley J M,De Deckkerb P,Roberts R G,et al.Optical dating of deep-sea sediments using single grains of quartz:a comparison with radiocarbon[J].Sedimentary Geology,2004,169:175-189.
[24]	Roberts R G,Bird M,Olley J M,et al.Optical and radiocarbon dating at Jimmium rock shelter in northern Australia[J].Nature,1998,393:358-362.
[25]	Olley J M,Caitcheon G,Murray A S.The distribution of apparent dose as determined by optically stimulated luminescence in small aliquots of fluvial quartz:implications for dating young sediments[J].Quat.Geochronol.,1998,17:1033-1040.
[26]	Ollerhead J,Huntley D J,Berger G W.Luminescence dating of the Buctouche Spit,New Brunswick[J].Canadian Journal of Earth Sciences,1994,31:523-531.
[27]	Huntley D J,Clague J J.Optical dating of tsunami-laid sands[J].Quaternary Research,1996,46:127-140.
[28]	Jeff Ollerhead,Huntley D J,Alan R Nelson,et al.Optical dating of tsunami-laid sand from an Oregon coastal lake[J].Quaternary Science Reviews,2001,20:1915-1926.
[29]	Price D M,Bryant E A,Young R W.Thermoluminescence evidence for the deposition of coastal sediments by tsunami wave action[J].Quaternary International,1999,56:123-128.
[30]	Alcina Magnolia,Franca Barreto,Francisco Hila,et al.Late Pleistocene marine terrace deposits in northeastern Brazil:sea-level change and tectonic implications[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2002,179:57-69.
[31]	Sytze van Heteren,David J Huntley,Orson van de Plassche Ronald K Lubberts.Optical dating of dune sand for the study of sea-level change[J].Geology,2000,28(5):411-414.
[32]	Murray A S,Clemmensen L B.Luminescence dating of Holocene sand movement,Thy,Denmark[J].Quaternary Science Reviews,2001,20:751-756.
[33]	Glenn W Berger,Andrew S Murray,Karen G Havholm.Photonic dating of Holocene back-barrier coastal dunes,northern North Carolina,USA[J].Quaternary Science Reviews,2003,22:1043-1050.
[34]	郑公望,朱忠礼.环境辐射场对热释光断代的影响[J].核技术,2001,24(12):1030-1032. [ZHENG Gong-wang,ZHU Zhong-li.Influence of the environmental radioactivities on TL dating[J].Nuclear Techniques,2001,24(12):1030-1032.]