Zobrazeno 1 - 8
of 8
pro vyhledávání: '"R. H. Steiger"'
Autor:
P. Stille, R. H. Steiger
Publikováno v:
Contributions to Mineralogy and Petrology. 107:273-278
First initial-Hf isotopic compositions for samples from the Alpine domain are presented and discussed. The results are mainly based on zircons and a few whole rocks with ages between 30 and 450 Ma. Of those so far analyzed, the present-day Hf isotopi
Publikováno v:
The Journal of Geology. 87:475-495
The southern part of the Caledonian fold belt in East Greenland comprises a complex of pre-Caledonian rock units as demonstrated by numerous age determinations and interpretation of field work. U-Pb isotopic age determinations on zircons, Rb-Sr analy
Publikováno v:
Rapport Grønlands Geologiske Undersøgelse. 134:5-18
Five new U-Pb age determinations on zireons and three new or reanalysed Rb-Sr age determinations of some of the late orogenie plutonic bodies from the Gåseland - Stauning Alper migmatite and granite zone in the Scoresby Sund region, give Caledonian
Autor:
P. D. Nunes, R. H. Steiger
Publikováno v:
Contributions to Mineralogy and Petrology. 47:255-280
U-Pb analyses of zircons from the southern paragneiss zone of the Gotthard massif in the central Alps indicate these rocks were derived from one or more source areas ≧ 1400 m.y. old and were strongly affected by both the Caledonian and Hercynian or
Publikováno v:
Bulletin of the Geological Society of Denmark. 29:151-160
Rb-Sr, U-Pb and K-Ar analyses on rocks and minerals from a tectonic window below a Caledonian thrust sheet in the westernmost part of the Scoresby Sund region (70°-72°N) give evidence for a Precambrian age of formation. The Charco't Land supracrust
Autor:
George R. Tilton, R. H. Steiger
Publikováno v:
Science. 150:1805-1808
Calculations based on comparison of the isotopic composition of lead from iron meteorites with that of various modern terrestrial leads have placed the age of the earth at around 4550 million years. However, recent data from young volcanic rocks reve
Autor:
R. H. Steiger, G. R. Tilton
Publikováno v:
Journal of Geophysical Research. 74:2118-2132
Granitic rocks at Manitouwadge, Ontario, have an age of 2720±50 m.y. based on isotopic lead data from zircon and sphene, and on Rb-Sr measurements from whole rocks. The rocks are stratigraphically and lithologically similar to ones called Algoman el
Publikováno v:
Contributions to Mineralogy and Petrology
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New Hornblende K-Ar and 39Ar-40Ar and mica Rb-Sr and K-Ar ages are used to place specific timemarks on a well-constrained pressure-temperature path for the late Alpine metamorphism in the Western Tauern Window. After identification of excess 40Ar the
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https://explore.openaire.eu/search/publication?articleId=doi_dedup___::288a92c0b0be8cec535beb56e070a04d
https://gfzpublic.gfz-potsdam.de/pubman/item/item_237639
https://gfzpublic.gfz-potsdam.de/pubman/item/item_237639