Detrital zircon U–Pb geochronology and provenance of the Late Quaternary sandstones in the Kumishi Basin, Northwest China: implication for intracontinental basin-range tectonic evolution-Reference-Cited by-同舟云学术

Detrital zircon U–Pb geochronology and provenance of the Late Quaternary sandstones in the Kumishi Basin, Northwest China: implication for intracontinental basin-range tectonic evolution

Published:2023-02-27 Issue:3 Volume:16 Page:
ISSN:1866-7511
Container-title:Arabian Journal of Geosciences
language:en
Short-container-title:Arab J Geosci

Author:

Yin Tiantao

Funder

The chemical exploration fund by China Chemical Geology and Mine Bureau

State Key Laboratory of Biogeology and Environmental Geology

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Environmental Science

Link

https://link.springer.com/content/pdf/10.1007/s12517-023-11276-6.pdf

Reference101 articles.

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2. Anderson T (2005) Detrital zircons as tracers of sedimentary provenance: limiting conditions from statistics and numerical simulation. Chem Geol 216:249–270

3. Armstrong-Altrin JS (2020) Detrital zircon U-Pb geochronology and geochemistry of the Riachuelos and Palma Sola beach sediments, Veracruz State, Gulf of Mexico: a new insight on palaeoenvironment. J Palaeogeogr 9:28

4. Armstrong-Altrin JS, RamosVázquez MA, Hermenegildo-Ruiz NY, Madhavaraju J (2020) Microtexture and U–Pb geochronology of detrital zircon grains in the Chachalacas beach, Veracruz State, Gulf of Mexico. Geol J. 1–21

5. Barbarin B (1999) A review of the relationships between granitoid types, their origins and their geodynamic environments. Lithos 46:605–626

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