Late Triassic tuff intervals in the Ordos basin, Central China: Their depositional, petrographic, geochemical characteristics and regional implications
Journal of Asian Earth Sciences（2014）
Abstract
•Late Triassic depositional events were activated by adjoining volcanism.•The Chang7 tuffs are derived from a calc-alkaline arc-related parental magma.•The Tianshui rhyolite is probably one of the volcanic sources of the Chang7 tuffs.
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Key words
Tuff intervals,Pyroclastic rocks,Event stratigraphy,Late Triassic,Ordos basin,Central China
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