Tracing the origin of zircon megacrysts in Triassic sediments of northeastern Siberian craton with implications to diamond paucity of craton-edge subcontinental lithospheric mantle

Author:

Skuzovatov Sergei,Wang Kuo-Lung,Smelov Alexander P.

Funder

Jarðvísindastofnun

Academia Sinica

Russian Foundation for Basic Research

Ministry of Science and Technology, Taiwan

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference86 articles.

1. U-Pb dating of zircons from alluvial and secondary deposits of the Yakutian diamondiferous province;Agashev;Ores and Metals,2019

2. Source rejuvenation vs. re-heating: Constraints on Siberian kimberlite origin from U–Pb and Lu–Hf isotope compositions and geochemistry of mantle zircons;Agashev;Lithos,2020

3. The subcontinental versus suboceanic debate, I lead-neodymium-strontium isotopes in primary alkali basalts from a shield area: the Ahaggar volcanic suite;Allègre;Earth Planet. Sci. Lett.,1981

4. Geochemistry of South African on and off-craton, group I and group II kimberlites: petrogenesis and source region evolution;Becker;J. Petrol.,2006

5. Igneous zircon: trace element composition as an indicator of source rock type;Belousova;Contrib. Mineral. Petrol.,2002

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