Extreme continental weathering in the northwestern Tethys during the end-Triassic mass extinction-Reference-Cited by-同舟云学术

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Extreme continental weathering in the northwestern Tethys during the end-Triassic mass extinction

Published:2022-05 Issue: Volume:594 Page:110934
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Onoue Tetsuji,Michalík Jozef,Shirozu Hideko,Yamashita Misa,Yamashita Katsuyuki,Kusaka Soichiro,Soda Katsuhito

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference163 articles.

1. Triassic–Jurassic weathering and clay mineral dispersal in basement areas and sedimentary basins of southern Sweden;Ahlberg;Sediment. Geol.,2003

2. The Statistical Analysis of Compositional Data;Aitchison,1986

3. Logistic-normal distributions: some properties and uses;Aitchison;Biometrika,1980

4. Introduction to Geochemical Modeling;Albarède,1995

5. Redox classification and calibration of redox thresholds in sedimentary systems;Algeo;Geochim. Cosmochim. Acta,2020

Cited by 7 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Norian (Upper Triassic) carbon isotopic perturbations and conodont biostratigraphy from the Simao terrane, eastern Tethys;Palaeogeography, Palaeoclimatology, Palaeoecology;2024-09

2. Weathering trends in the Norian through geochemical and rock magnetic analyses from the Pignola–Abriola section (Lagonegro Basin, Italy);Climate of the Past;2024-03-22

3. Marine Strontium Isotope Evolution at the Triassic‐Jurassic Transition Links Transient Changes in Continental Weathering to Volcanism of the Central Atlantic Magmatic Province;Geochemistry, Geophysics, Geosystems;2024-03

4. Rhenium-osmium isotope evidence for the onset of volcanism in the central Panthalassa Ocean during the Norian “chaotic carbon episode”;Global and Planetary Change;2023-10

5. Provenance of quartz debris in the Central Western Carpathians at the end of the Triassic, as indicated by cathodoluminescence colours;Acta Geologica Polonica;2023-07-26

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