SURFACE EXPOSURE DATING - REVIEW AND CRITICAL-EVALUATION

被引:21
作者
DORN, RI
PHILLIPS, FM
机构
[1] Department of Geography, Arizona State University, Tempe, AZ
[2] Department of Geoscience, New Mexico Tech, Socorro, NM
基金
美国国家科学基金会;
关键词
Cosmogenic nuclides; Geochronology; Geomorphology; Process; Quaternary; Rock varnish; Soils; Surface exposure dating; Weathering;
D O I
10.1080/02723646.1991.10642436
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The past decade has seen the development and application of over a dozen new methods for quantitative age-determinations of geomorphic surfaces. Some surface exposure dating methods are numerical, including the accumulation of cosmogenic radionuclides Be-10, C-14, Al-26, Cl-36, and Ca-41, accumulation of cosmogenic stable nuclides He-3 and Ne-21, C-14 dating of organic matter encapsulated in rock coatings, and dendrogeomorphology. Calendar ages are obtained by dendrogeomorphological analysis. Calibrated ages can be obtained by analysis of rock-varnish chemistry, lichenometry, weathering, and soils. Various methods can be used in combination to overcome individual limitations. Whereas conventional methods provide age control on stratigraphic profiles, surface-exposure dating methods are especially suitable for geographic problems, such as analyzing not only temporal, but also spatial variations in the rates of geomorphic processes.
引用
收藏
页码:303 / 333
页数:31
相关论文
共 205 条
[1]  
Colman S.M., Pierce K.L., Birkeland P.W., Suggested terminology for quaternary dating methods, Quaternary Research, 28, pp. 314-319, (1987)
[2]  
Elliott-Fisk D.L., Glacial geomorphology of the white mountains, california and nevada: Establishment of a glacial chronology, Physical Geography, 8, pp. 299-323, (1987)
[3]  
Gerson R., Talus relicts in deserts: A key to major climatic fluctuations, Israel Journal of Earth Science, 31, pp. 123-132, (1982)
[4]  
Gibbons A.B., Megeath J.D., Pierce K.L., Probability of moraine survival in a succession of glacial advances, Geology, 12, pp. 327-330, (1984)
[5]  
Gilbert G.K., Lake bonneville, U.S. Geological Survey Monograph, 1, pp. 1-438, (1890)
[6]  
Oviatt C.G., Currey D.R., Miller D.M., Age and paleoclimatic significance of the stansbury shoreline of lake bonneville, northeastern great basin, Quaternary Research, 33, pp. 291-305, (1990)
[7]  
Schmidt K., The significance of scarp retreat for cenozoic landform evolution on the colorado plateau, usa, Earth Surface Processes and Landforms, 14, pp. 93-105, (1989)
[8]  
Ahnert F., Modelling landform change, Modelling Geomorphological Systems, pp. 375-400, (1988)
[9]  
Bucknam R.C., Anderson R.E., Estimation of fault-scarp ages from a scarp-height slope-angle relationship, Geology, 7, pp. 11-14, (1979)
[10]  
Coates D.R., Landforms and landscapes as measures of relative age, Quaternary Dating Methods, pp. 247-267, (1984)