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Volumn 8, Issue 1, 1970, Pages 169-198

Insolation changes, ice volumes, and the O18 record in deep‐sea cores

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Indexed keywords


EID: 84995072197     PISSN: 87551209     EISSN: 19449208     Source Type: Journal    
DOI: 10.1029/RG008i001p00169     Document Type: Review
Times cited : (592)

References (48)
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    • Paleotemperature analysis of Caribbean cores P6304–8 and P6304–9 and a generalized temperature curve for the past 425,000 years
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    • Emiliani, C.1
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    • Caribbean cores P6304–8 and P6304–9: New analysis of absolute chronology, A reply
    • (1969) Science , vol.166 , pp. 1551
    • Emiliani, C.1    Rona, E.2
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    • Sea‐level changes during the last 10,000 yearsProceedings of the Intern. Symposium on World Climate from 8000 to O B.C., p. 54Royal Meteorological Society
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    • Jelgersma, S.1
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    • 0003397019 scopus 로고
    • Uranium series disequilibrium in deep sea sediments
    • Ph.D. thesis, Columbia University
    • (1966)
    • Ku, T.L.1
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    • Atlantic deep‐sea stratigraphy: extension of absolute chronology to 320.000 years
    • (1966) Science , vol.161 , pp. 448
    • Ku, T.L.1    Broecker, W.S.2
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    • The problem of sample contamination in radiocarbon dating
    • Ph.D. thesis, Columbia University
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    • Olson, E.A.1
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    • Oxygen isotope analyses and Pleistocene temperatures re‐assessed
    • (1967) Nature , vol.216 , pp. 15
    • Shackleton, N.1
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    • Long‐period global variations of incoming solar radiation, Research on the Theory of Climate, vol. 2, 289, report of the Travelers Research Center, Inc., Hartford, Conn., May
    • (1968)
    • Vernekar, A.D.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.