R V Krishnamurthy

Datos Biográficos

ID3528674
NOMBRER V Krishnamurthy
NOMBRESR V
APELLIDOKrishnamurthy
FIRMAKRISHNAMURTHY R V
VERIFICADONo
TOTAL DE OBRAS10
TOTAL DE CITAS7
TOTAL COMO AUTOR10
TOTAL COMO EDITOR0
PRIMER AÑO DE PUBLICACIÓN1976
AÑO MÁS RECIENTE DE PUBLICACIÓN2011
ÍNDICE H2

  • Monsoon variability and chemical weathering during the late Pleistocene in the Goriganga basin, higher central Himalaya, India

    Open AccessSteven P Beukema, R V Krishnamurthy et al.ARTICLEQuaternary Research2011

    Stable isotope analysis along with radiocarbon and luminescence dating of late Pleistocene lacustrine deposits at Burfu in the higher central Himalaya are used to interpret hydrologic changes in the lake basin. From 15.5 ka to ~ 14.5 ka the Burfu lake was largely fed by melting glaciers. A warming event at 14.5 ka suggests an enhanced monsoon and increased carbonate weathering. From ~ 13.5 ka to ~ 12.5 ka the isotopic data suggest large-amplitude…

  • Inferring paleotemperature from the D/H ratio of lacustrine organic matter

    Open AccessNorman A Lovan, R V KrishnamurthyARTICLEQuaternary International2011

  • Physical Research Laboratory Radiocarbon Date List V

    Open AccessD P Agrawal, R V Krishnamurthy et al.ARTICLERadiocarbon1985Citada por: 2Referencias: 1

    We report here dates on archaeologic and geologic samples. The samples were counted as methane in gas proportional counters. The techniques used have been described earlier (R, 1971, v 13, p 442–449). Dates are expressed in years BP, taking AD 1950 as the reference year. Modern standard was NBS oxalic acid. Quoted errors are based on counting statistics alone and are equivalent to ±1 standard deviation for samples younger than 10,000 years and ± …

  • Late Quaternary Faunal Change in Coastal Arabian Sea Sediments

    Open AccessD V Borole, K Kameswara Rao et al.ARTICLEQuaternary Research1982

    Carbonate content and faunal composition of two gravity cores from the coastal Arabian sea provide evidence of a major environmental change in surface ocean waters about 13,000 yr B.P. Radiocarbon dating indicates that deposition rates ranged from 1.8 to 9.8 cm/10 3 yr, with a major change in rate occurring in one core at about 7500 yr B.P.

  • Physical Research Laboratory Radiocarbon Date List IV

    Open AccessD P Agrawal, R V Krishnamurthy et al.ARTICLERadiocarbon1981Referencias: 1

    The dates presented below are from some important archaeologic and Quaternary sites. All the dates are in years bp, based on τ1⁄2 = 5568 years. When converting archaeologic dates into the ad/bc scale, 1950 should be used as the base year. The dates are not corrected for 13 C fractionation. All the dates older than 10,000 years have been given with 2σ errors

  • Studies On the Loess Deposits of the Kashmir Valley and 14 C Dating

    Open AccessSheela Kusumgar, D P Agrawal et al.ARTICLERadiocarbon1980Citada por: 3Referencias: 2

    The loessic deposits along with their palaeosols of the Kashmir Valley have been 14 C dated using both organic and carbonate fractions. The 14 C dates on both the fractions show good concordance. The 14 C dates indicate that the last deglaciation in Kashmir (34° N) already started CA 18,000 ± 1000 BP at CA 1600m and CA 15,000 BP at CA 3000m altitude and thus support the recent global evidence of deglaciation having started several millennia befor…

  • Physical Research Laboratory Radiocarbon Date List III

    Open AccessD P Agrawal, R V Krishnamurthy et al.ARTICLERadiocarbon1978Referencias: 2

    Presented below are dates from some important archaeologic and Quaternary sites. All dates are based on τ 1⁄2 = 5568 yr; to convert the radiocarbon dates for archaeologic samples into ad/bc scale, 1950 has been used as base as per the resolution passed at the Ninth International Radiocarbon Conference, San Diego, 1976. The dates are not corrected for 13 C fractionation. All the dates older than 10,000 yr have been given with 2σ errors. Due to unc…

  • Chronology of Indian prehistory from the Mesolithic period to the Iron Age

    Open AccessD P Agrawal, R V Krishnamurthy et al.ARTICLEJournal of Human Evolution1978Citada por: 1Referencias: 3

  • Physical Research Laboratory Radiocarbon Date List II

    Open AccessD P Agrawal, R V Krishnamurthy et al.ARTICLERadiocarbon1977Referencias: 1

    Presented below are dates from some important archaeologic and Quaternary sites. For the first time, a large number of dates have been reported here on the eustatic changes on the Eastern Indian coast. All dates are based on τ 1/2 — 5568 yr; to convert the radiocarbon dates for archaeological samples into ad/bc scale, 1950 has been used as base year as per resolution passed at the Ninth International Radiocarbon Conference, San Diego, 1976. The d…

  • Physical Research Laboratory Radiocarbon Date List I

    Open AccessD P Agrawal, R V Krishnamurthy et al.ARTICLERadiocarbon1976Citada por: 1Referencias: 1

    As the Radiocarbon Lab of the Tata Institute, Bombay, has now been shifted to the Physical Research Laboratory (PRL), Ahmedabad, our new date lists will be termed as above and the samples will be given PRL numbers instead of the former TF. All the pending TF samples were given new PRL numbers