Hidden Eoarchean crust in the southwestern Central Asian Orogenic Belt-Reference-Cited by-同舟云学术

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Hidden Eoarchean crust in the southwestern Central Asian Orogenic Belt

Published:2020-05 Issue: Volume:360-361 Page:105437
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Wang Jian,Su Yuping,Zheng Jianping,Belousova E.A.,Griffin W.L.,Zhou Xiang,Dai Hongkun

Funder

National Natural Science Foundation of China

Fundamental Research Funds for the Central Universities

University of Geosciences

CUG

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference82 articles.

1. Ti-U-Th-Pb depth profiling of Hadean zircons: a search for evidence of ancient extraterrestrial impacts;Abbott;Proc. Natl. Acad. Sci.,2012

2. Nature of the Earth’s earliest crust from hafnium isotopes in single detrital zircons;Amelin;Nature,1999

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

4. Age and compositional data of zircon from sepiolite drilling mud to identify contamination of ocean drilling samples;Andrews;Geochem. Geophys. Geosyst.,2016

5. Post-Hadean transitions in Jack Hills zircon provenance: a signal of the late heavy bombardment?;Bell;Earth Planet. Sci. Lett.,2013

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2. A Late Palaeozoic disconformity in the Moqinwula area: Insights into the tectonic evolution and basement nature of the Junggar Block, NW China;Geological Journal;2023-04-04

3. Voluminous continental growth of the Altaids and its control on metallogeny;National Science Review;2022-12-19

4. Archean to Paleoproterozoic crustal evolution of the southern Yangtze Block (South China): U–Pb age and Hf-isotope of zircon xenocrysts from the Paleozoic diamondiferous kimberlites;Precambrian Research;2022-06

5. The delamination of lower crust in continental back-arc basin: Evidence from Sr isotope and elemental compositions of plagioclase and clinopyroxene in andesites from Kueishantao, north of Taiwan, China;Lithos;2022-05

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