The effect of mineral age discordancies on total-rock Rb-Sr isochrons of the Heemskirk Granite, western Tasmania-Reference-Cited by-同舟云学术

The effect of mineral age discordancies on total-rock Rb-Sr isochrons of the Heemskirk Granite, western Tasmania

Published:1966-11-15 Issue:22 Volume:71 Page:5447-5458
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

Brooks C.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Link

http://www.agu.org/journals/jz/v071/i022/JZ071i022p05447/JZ071i022p05447.pdf

Reference9 articles.

1. The discordance of mineral ages in granitic rocks resulting from the redistribution of Rb and Sr;Arriens;J. Geophys. Res.,1966

2. Rb-Sr ages of some Tasmanian granitic rocks;Brooks;J. Geol. Soc. Australia,1966

3. The age and initial Sr87/Sr86 of the Heemskirk granite, western Tasmania;Brooks;J. Geophys. Res.,1965

4. The Rb-Sr age of the Bishopville aubrite and its component enstatite and feldspar;Compston;Geochim. Cosmochim. Acta,1965

5. K-feldspar structural states as petrogenic indicators;Dietrich;Norsk. Geol. Tidsskr.,1962

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