Formation of Ediacaran stromatolitic cherts through a combination of biogenic and abiotic processes: New insights from the Bohemian Massif
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Elsevier BV
Reference89 articles.
1. Architecture and composition of ocean floor subducted beneath northern Gondwana during Neoproterozoic to Cambrian: a palinspastic reconstruction based on Ocean Plate Stratigraphy (OPS);Ackerman;Gondwana Res.,2019
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3. The significance of cherts as markers of Ocean Plate Stratigraphy and paleoenvironmental conditions: new insights from the Neoproterozoic-Cambrian Blovice accretionary wedge, Bohemian Massif;Ackerman;Geosci. Front.,2023
4. Seawater silica cycling and chert formation at the Neoproterozoic-Cambrian transition: insights from δ30Si and Ge/Si systematics of hydrothermal cherts from the Bohemian Massif;Ackerman;Chem. Geol.,2023
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