Late Triassic (Norian) strontium and oxygen isotopes from the Baoshan block, southwestern China: Possible causes and implications for climate change-Reference-Cited by-同舟云学术

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Late Triassic (Norian) strontium and oxygen isotopes from the Baoshan block, southwestern China: Possible causes and implications for climate change

Published:2024-09 Issue: Volume:650 Page:112378
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Chen Yan,Zeng Weiping,Joachimski Michael M.,Wignall Paul B.,Ogg James G.,Jiang Haishui,Zhang Muhui,Lai Xulong

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Reference121 articles.

1. Onshore climate change during the late Triassic marine inundation of the central European Basin;Ahlberg;Terra Nova,2002

2. Palaeomagnetic re-investigation of early Permian rift basalts from the Baoshan Block, SW China: Constraints on the site-of-origin of the Gondwana-derived eastern Cimmerian terranes;Ali;Geophys. J. Int.,2013

3. Thermal effects on rare earth element and strontium isotope chemistry in single conodont elements;Armstrong;Geochim. Cosmochim. Acta,2001

4. The evolution of the Triassic rift basin in the Baoshan Block of Western Yunnan;Bao;Adv. Geosci.,2020

5. Norian vegetation history and related environmental changes: New data from the Chinle Formation, Petrified Forest National Park (Arizona, SW USA);Baranyi;GSA Bull.,2018

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