U–Pb geochronology and REE geochemistry of zircons from Palaeoproterozoic paragneiss clasts in the Mesozoic Kamiaso conglomerate, central Japan: evidence for an Archean provenance-Reference-Cited by-同舟云学术

U–Pb geochronology and REE geochemistry of zircons from Palaeoproterozoic paragneiss clasts in the Mesozoic Kamiaso conglomerate, central Japan: evidence for an Archean provenance

Published:2002-08 Issue:3-4 Volume:187 Page:279-293
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Hidaka Hiroshi,Shimizu Hiroshi,Adachi Mamoru

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference39 articles.

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2. Pelitic and quartzo-feldspathic gneisses in the Kamiaso conglomerate: a study of Precambrian geology in Japan and East Asia;Adachi;J. Geol. Soc. Jpn.,1973

3. Were Precambrian gneiss clasts in the Kamiaso conglomerate derived from the eastern Korea Peninsula?;Adachi;Bull. Nagoya Univ. Furukawa Mus.,1993

4. 3800 to 2500 Ma crustal evolution in the Anshan area of Liaoning Province, northeastern China;Biao;Precambrian Res.,1996

5. Crustal evolution of southeastern China: Nd and Sr isotopic evidence;Chen;Tectonophysics,1998

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