Paleozoic tectonic evolution of the proto-Korean Peninsula along the East Asian continental margin from detrital zircon U-Pb geochronology and Hf isotope geochemistry-Reference-Cited by-同舟云学术

Paleozoic tectonic evolution of the proto-Korean Peninsula along the East Asian continental margin from detrital zircon U-Pb geochronology and Hf isotope geochemistry

Published:2024-01 Issue:1 Volume:15 Page:101700
ISSN:1674-9871
Container-title:Geoscience Frontiers
language:en
Short-container-title:Geoscience Frontiers

Author:

Jang Yirang,Kim Sung Won,Samuel Vinod O.,Kwon Sanghoon,Park Seung-Ik,Santosh M.,Yi Keewook

Funder

MOTIE

Korea Basic Science Institute

National Research Foundation of Korea

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences

Reference135 articles.

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2. Early-middle Archaean crustal evolution deduced from Lu–Hf and U-Pb isotopic studies of single zircon grains;Amelin;Geochim. Cosmochim. Acta,2000

3. The zircon U-Pb and Hf isotope constraints on the basement nature and Paleozoic evolution in northern margin of Yili Block, NW China;An;Gondw. Res.,2017

4. Detrital zircon in an active sedimentary recycling system: Challenging the ‘source-to-sink’ approach to zircon-based provenance analysis;Andersen;Sedimentology,2022

5. The U-Pb and Hf isotope evidence of detrital zircons of the Ordovician Ollantaytambo Formation, southern Peru, and the Ordovician provenance and paleogeography of southern Peru and northern Bolivia;Bahlburg;J. S. Am. Earth Sci.,2011

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