Zobrazeno 1 - 10
of 11
pro vyhledávání: '"J. F. Sutter"'
Autor:
Yu. A. Shukolyukov, K. Wetzel, H. J. Lippolt, M. I. Karpenko, J. F. Sutter, D. J. DePaolo, T. F. Anderson, V. I. Vinogradov, E. V. Bibikova, J. N. Aleinikoff, M. Ozima, I. V. Chernyshev, B. L. Gulson, J. R. O’Neil, E. M. Galimov, J. Hoefs, B. G. Pokrovsky, D. Rumble, D. Haendel
Publikováno v:
Methods and Instrumentations: Results and Recent Developments ISBN: 9783642785283
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::18b0c40d79d122a8b935150be8f9310d
https://doi.org/10.1007/978-3-642-78526-9_8
https://doi.org/10.1007/978-3-642-78526-9_8
Autor:
J. F. Sutter, R. D. Dallmeyer
Publikováno v:
American Journal of Science. 276:731-747
Autor:
J. F. Sutter, T. E. Smith
Publikováno v:
American Journal of Science. 279:808-831
Autor:
J. F. Sutter, Robert P. Wintsch
Publikováno v:
The Journal of Geology. 94:459-472
Hornblende and biotite /sup 40/Ar//sup 39/Ar age spectra from rocks in south-central Connecticut help define a Permian-Triassic cooling curve for the area. Together with petrologic and structural information, a time-temperature-pressure-strain path i
Publikováno v:
American Journal of Science. 287:635-660
Publikováno v:
Earth and Planetary Science Letters. 11:249-253
High temperature 40 Ar/ 39 Ar ages have been determined for four rock fragments selected from coarse fines returned from Fra Mauro. Three are fragmental rocks in varying stages of recrystallization and the fourth is crystalline with a gabbro mineralo
Publikováno v:
Canadian Journal of Earth Sciences. 8:1495-1498
Hornblende-rich concentrates from quartz–feldspar gneisses of the Grenville Province near Brent Ontario, have yielded K–Ar apparent ages of 1570 to 1480 ± 80 m.y., while coexisting biotite- and feldspar-rich separates give 'normal' Grenville K
Autor:
C. H. Anderson, J. F. Sutter
Publikováno v:
Journal of Aircraft. 4:452-456
Publikováno v:
Science (New York, N.Y.). 175(4023)
In their report on the ages of crystalline rocks from the Apollo 14 mission, Husain, Sutter, and Schaeffer present some important results using the ^(40)Ar-^(39)Ar method. This technique, which has been used by several other workers, depends critical
Publikováno v:
Science. 173:1235-1236
Crystallization ages for six rocks from Fra Mauro have been measured by the argon-40-argon-39 method. All six rocks give an age of 3.77 +/- 0.15 x 10(9) years, which is the same as for fragmental rocks from this site. It is concluded that the Imbrium