D. Kharkar

发表

Slow growth rate of a deep-sea clam determined by 228Ra chronology.

K. Turekian, J. Vaisnys, J. Cochran, 1975, Proceedings of the National Academy of Sciences of the United States of America.

‘Dating’ Ground Waters of Ages Younger than 1,000–1,500 Years Using Natural Silicon-32

D. Lal, D. Kharkar, V. Nijampurkar, 1966, Nature.

The global fallout of Si 32 produced by cosmic rays

D. Lal, D. Kharkar, V. Nijampurkar, 1966 .

Comparison of sedimentation rates obtained by32Si and uranium decay series determinations in some siliceous Antarctic cores

K. Turekian, M. R. Scott, D. Kharkar, 1969 .

Uranium and thorium decay series nuclides in plankton from the Caribbean1

K. Turekian, J. Thomson, D. Kharkar, 1976 .

Cosmogenic 10 Be and 26 Al in marine sediments

D. Kharkar, B. S. Amin, D. Lai, 1966 .

The beryllium-10 concentration in deep-sea sediments

P. S. Goel, D. Lal, D. Kharkar, 1957 .

Stream supply of dissolved silver, molybdenum, antimony, selenium, chromium, cobalt, rubidium and cesium to the oceans

K. Turekian, K. Bertine, D. Kharkar, 1968 .

Spectrophotometric determination of titanium after separation by anion exchange

G. Arrhenius, D. Kharkar, J. Korkisch, 1963 .

Uranium and Thorium Decay Series Nuclide Abundances in Marine Plankton

K. Turekian, J. Thomson, D. Kharkar, 1973 .

Prehistoric cosmic ray intensity

P. S. Goel, D. Lal, D. Kharkar, 1958 .

Cosmic ray produced Mg 28 , Si 31 , S 38 , Cl 38 , Cl 34m and other short-lived radioisotopes in wet precipitation

D. Lal, A. S. Tamhane, N. Bhandari, 1966 .

COSMIC RAY PRODUCED $sup 28$Mg, $sup 31$Si, $sup 38$S, $sup 38$Cl, /sup 34m/ Cl, AND OTHER SHORT-LIVED RADIOISOTOPES IN WET PRECIPITATION.

D. Lal, A. S. Tamhane, N. Bhandari, 1966 .

An evaluation of the uranium-helium method of dating of fossil bones

K. Turekian, D. Kharkar, J. Funkhouser, 1970 .

Obsidian trade at san lorenzo tenochtitlan, Mexico.

M. Coe, K. Turekian, D. Kharkar, 1971, Science.

Peroxy titanium oxalate

C. Patel, D. Kharkar, 1956 .

Neutron Activation Analysis of Milligram Quantifies of Lunar Rocks and Soils

K. Turekian, D. Kharkar, 1970, Science.

Slow growth rate of a deep-sea clam determined by 228 Ra chronology ( growth bands / ages of deep-dwelling organisms with hard parts )

K. Turekian, J. Vaisnys, R. Cerrato, 2003 .