Dating sediment burial with in situ-produced cosmogenic nuclides: theory, techniques, and limitations

被引:368
作者
Granger, DE [1 ]
Muzikar, PF
机构
[1] Purdue Univ, Dept Earth & Atmospher Sci, Prime Lab, W Lafayette, IN 47907 USA
[2] Purdue Univ, Dept Phys, W Lafayette, IN 47907 USA
基金
美国国家科学基金会;
关键词
cosmogenic elements; geochronology; burial; sediments;
D O I
10.1016/S0012-821X(01)00309-0
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Dating sediment burial over million-year time scales is crucial in many areas of the Earth sciences and archeology, but is often difficult using traditional techniques. Sediment burial can be dated by the radioactive decay of cosmogenic nuclides, provided that the sediment was exposed to cosmic rays prior to burial. Dating calculations are straightforward if sediment is buried deeply and rapidly enough to prevent cosmogenic nuclide production after burial. However. the analysis can be complicated by postburial production if sediment is insufficiently shielded from secondary cosmic-ray nucleons and muons. This paper discusses how buried sediments can be dated over timescales up to 5 Myr using Al-26 and Be-10 in quartz. (C) 2001 Published by Elsevier Science B.V.
引用
收藏
页码:269 / 281
页数:13
相关论文
共 35 条
[1]   Be-10 and Al-26 evidence for exceptionally low rates of Australian bedrock erosion and the likely existence of pre-pleistocene landscapes [J].
Bierman, P ;
Turner, J .
QUATERNARY RESEARCH, 1995, 44 (03) :378-382
[3]   Mid-Pleistocene cosmogenic minimum-age limits for pre-Wisconsinan glacial surfaces in southwestern Minnesota and southern Baffin island: a multiple nuclide approach [J].
Bierman, PR ;
Marsella, KA ;
Patterson, C ;
Davis, PT ;
Caffee, M .
GEOMORPHOLOGY, 1999, 27 (1-2) :25-39
[4]   FLUX OF THE VERTICAL NEGATIVE MUONS STOPPING AT DEPTHS 0.35-1000 HG CM2 [J].
BILOKON, H ;
CASTAGNOLI, GC ;
CASTELLINA, A ;
PIAZZOLI, BD ;
MANNOCCHI, G ;
MERONI, E ;
PICCHI, P ;
VERNETTO, S .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1989, 94 (B9) :12145-12152
[5]   EVIDENCE FOR MUON-INDUCED PRODUCTION OF BE-10 IN NEAR-SURFACE ROCKS FROM THE CONGO [J].
BROWN, ET ;
BOURLES, DL ;
COLIN, F ;
RAISBECK, GM ;
YIOU, F ;
DESGARCEAUX, S .
GEOPHYSICAL RESEARCH LETTERS, 1995, 22 (06) :703-706
[6]   EFFECTIVE ATTENUATION LENGTHS OF COSMIC-RAYS PRODUCING BE-10 AND AL-26 IN QUARTZ - IMPLICATIONS FOR EXPOSURE AGE DATING [J].
BROWN, ET ;
BROOK, EJ ;
RAISBECK, GM ;
YIOU, F ;
KURZ, MD .
GEOPHYSICAL RESEARCH LETTERS, 1992, 19 (04) :369-372
[7]   GEOMORPHOLOGY AND IN-SITU COSMOGENIC ISOTOPES [J].
CERLING, TE ;
CRAIG, H .
ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, 1994, 22 :273-317
[8]   Quantifying passive margin denudation and landscape development using a combined fission-track thermochronology and cosmogenic isotope analysis approach [J].
Cockburn, HAP ;
Brown, RW ;
Summerfield, MA ;
Seidl, MA .
EARTH AND PLANETARY SCIENCE LETTERS, 2000, 179 (3-4) :429-435
[9]   Scaling factors for production rates of in situ produced cosmogenic nuclides: a critical reevaluation [J].
Dunai, TJ .
EARTH AND PLANETARY SCIENCE LETTERS, 2000, 176 (01) :157-169
[10]  
Gosse J., 2001, EOS, V82, P82