Zobrazeno 1 - 10
of 61
pro vyhledávání: '"Tatsumoto,Mitsunobu"'
Autor:
Basu, Asish R., Tatsumoto, Mitsunobu
Publikováno v:
Science, 1979 Jul . 205(4404), 398-401.
Externí odkaz:
https://www.jstor.org/stable/1748090
Publikováno v:
Science, 1975 Oct 01. 190(4210), 143-147.
Externí odkaz:
https://www.jstor.org/stable/1740943
Publikováno v:
Science, 1985 Oct . 230(4724), 436-439.
Externí odkaz:
https://www.jstor.org/stable/1696079
Time Differences in the Formation of Meteorites as Determined from the Ratio of Lead-207 to Lead-206
Publikováno v:
Science, 1973 Jun . 180(4092), 1279-1283.
Externí odkaz:
https://www.jstor.org/stable/1736131
Autor:
Nunes, P. D., Tatsumoto, Mitsunobu
Publikováno v:
Science, 1973 Nov . 182(4115), 916-920.
Externí odkaz:
https://www.jstor.org/stable/1737739
Publikováno v:
Limnology and Oceanography, 1960 Oct 01. 5(4), 425-431.
Externí odkaz:
https://www.jstor.org/stable/2832488
Autor:
Tatsumoto, Mitsunobu, Rosholt, John N.
Publikováno v:
Science, 1970 Jan . 167(3918), 461-463.
Externí odkaz:
https://www.jstor.org/stable/1728714
Autor:
Morikawa,Noritoshi, Misawa,Keiji, Kondorosi,Gabor, Premo,Wayne R., Tatsumoto,Mitsunobu, Nakamura,Noboru
Publikováno v:
Antarctic meteorite research. 14:47-60
We have undertaken a Rb-Sr isotopic study of the lherzolitic shergottite, Yamato (Y)-793605. The acid-leaching experiment designed to remove secondary Pb contamination during previous work with U-Th-Pb systematics did not significantly affect the Rb-
Publikováno v:
Antarctic meteorite research. 10:95-108
We have undertaken U-Th-Pb isotopic studies on lherzolitic shergottite, Yamato-793605. Four mineral separates (olivine, plagioclase, and two phases of pyroxene) and a whole-rock sample were leached with dilute acid in order to remove secondary Pb con
Publikováno v:
Proceedings of the NIPR Symposium on Antarctic Meteorites. 6:58-75
U-Th-Pb isotopic data were determined on mineral separates of the diabasic lunar meteorite, Yamato-793169,in order to define its age and characterize its magma source. Such results have been helpful toward our understanding of the magmatic/chemical e