Detrital zircon U-Pb geochronology of Ordovician-Silurian strata in the northwestern platform of the Tarim Basin: Implications for provenance systems and tectonic evolution-Reference-Cited by-同舟云学术

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Detrital zircon U-Pb geochronology of Ordovician-Silurian strata in the northwestern platform of the Tarim Basin: Implications for provenance systems and tectonic evolution

Published:2024-10 Issue: Volume:134 Page:1-20
ISSN:1342-937X
Container-title:Gondwana Research
language:en
Short-container-title:Gondwana Research

Author:

Zhong Ziqi,Hou Guiting,Xia Jinkai,Li Xiang,Wei Lunyan,Chang Haining^ORCID

Publisher

Elsevier BV

Reference167 articles.

1. The Lu-Hf geochemistry of chondrites and evolution of the mantle-crust system;Blichert-Toft;Earth Planet. Sci. Lett.,1997

2. An 800-million-year detrital zircon record of continental amalgamation: Tarim basin;Carroll;NW China. Int. Geol. Rev.,2013

3. Provenance record of a rift basin: U/Pb ages of detrital zircons from the Perth basin, western Australia;Cawood;Sed. Geol.,2000

4. Analysis of proto-type Tarim Basin in the late Precambrian and the dynamic mechanism of its evolution;Chang;Plos One,2023

5. Tectono-thermal evolution of the northwestern edge of the Tarim Basin in China: constraints from apatite (U-Th)/He thermochronology;Chang;J. Asian Earth Sci.,2012

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1. Helium Geochemical Characteristics and Favorable Zones in the Tarim Basin: Implications for Helium Exploration;Processes;2024-07-13

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