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Volumn 274, Issue 5288, 1996, Pages 749-751

Chronology for fluctuations in late Pleistocene Sierra Nevada glaciers and lakes

Author keywords

[No Author keywords available]

Indexed keywords

CHLORINE 36;

EID: 0029660256     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.274.5288.749     Document Type: Article
Times cited : (166)

References (32)
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    • 36Cl production by neutrons from U and Th in the rock was calculated using the approach of J. T. Fabryka-Martin [thesis, University of Arizona (1988)].
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  • 17
    • 10544219725 scopus 로고    scopus 로고
    • note
    • 14C kyr = 1000 carbon-14 years)
  • 18
    • 0028593233 scopus 로고
    • 36Cl by thermal neutrons, which counters age bias due to rock weathering; (ii) the average size of boulders we sampled (1 to 4 m) was much larger than they assumed (0.5 m); and (iii) even if their analysis were correct, the effects would be small in the age range considered here [figure 2B of (25)].
    • (1994) Water Resour. Res. , vol.30 , pp. 3127
    • Zreda, M.G.1    Phillips, F.M.2    Elmore, D.3
  • 20
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    • 3He ages of 27 and 20.5 ka obtained at June Lake [R. J. Poreda et al., Eos 76 (fall suppl.), 685 (1995)].
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    • By "modern" surface area of Owens Lake we mean before the major diversion of Owens River in 1913.
    • By "modern" surface area of Owens Lake we mean before the major diversion of Owens River in 1913.
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    • thesis, New Mexico Institute of Mining and Technology
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    • note
    • We thank R. Dorn, D. Elliot-Fisk, S. S. Smith, and M. Flinsch. Support was provided by the Geography, Geoscience, and Physics divisions of NSF.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.