Ion microprobe UPb zircon geochronology and isotopic evidence for a trans-crustal suture in the Lapland–Kola Orogen, northern Fennoscandian Shield-Reference-Cited by-同舟云学术

Ion microprobe UPb zircon geochronology and isotopic evidence for a trans-crustal suture in the Lapland–Kola Orogen, northern Fennoscandian Shield

Published:2001-01 Issue:2-4 Volume:105 Page:289-314
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Daly J.S,Balagansky V.V,Timmerman M.J,Whitehouse M.J,de Jong K,Guise P,Bogdanova S,Gorbatschev R,Bridgwater D

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference80 articles.

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2. Kinematics of movements in some structural zones in the Kola Precambrian;Balagansky,1992

3. Balagansky, V.V., Bogdanova, M.N., Kozlova, N.Ye., 1986. Structural and Metamorphic Evolution of the Northwestern Belomorian Region (in Russian). Kola Branch of USSR Acad. Sci, Apatity 100 pp.

4. The early Proterozoic evolution of the northeastern Baltic Shield: a terrane analysis;Balagansky;Geotektonika (in Russian),1998

5. Isotopic age of rocks from the Kolvitsa Belt and the Umba block (the southeastern extension of the Lapland Granulite Belt), Kola Peninsula;Balagansky;Proc. Murmansk State Tech. Univ. (in Russian),1998

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