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A geochemical view into continental palaeotemperatures of the end-Permian using oxygen and hydrogen isotope composition of secondary silica in chert rubble breccia: Kaibab Formation, Grand Canyon (USA)

Crossref DOI link: https://doi.org/10.1186/s12932-017-0047-y

Published Online: 2018-01-16

Published Print: 2018-12

Update policy: https://doi.org/10.1007/springer_crossmark_policy

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