Olistolith (to the left) of the destructured red clay-marl

Rifting of Columbia to form a deep-water siliciclastic to carbonate succession: The Mesoproterozoic Pinguicula Group of northern Yukon, Canada - ScienceDirect

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Rifting of Columbia to form a deep-water siliciclastic to carbonate succession: The Mesoproterozoic Pinguicula Group of northern Yukon, Canada - ScienceDirect

PDF) GEOLOGICAL ENVIRONMENTS FORMING THE EOCENE BLACK-SHALE FORMATION OF THE SILESIAN NAPPE (UKRAINIAN CARPATHIANS)

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