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Figure 5. Inferred structure of the Batenev intraoceanic mount of Vendian-Middle Cambrian age.
(1) Varved limestone with a high Ba content in the lower rocks of the Middle Cambrian; (2) tuffite, ash-bearing limestone, and carbonaceous-siliceous shale (a); same in shallow-sea rocks (b); (3) ash limestone of conglomerate and breccia structure in the upper interval of the Lower Cambrian; (4) carbonaceous limestone in the upper part of the Lower Cambrian; (5) bioclastic and reef limestone at the base of the Lower Cambrian; (6) dolomitized calcarenite and calcilutite with interlayers of oncolite and fenestrate varieties (a) and interlayers of organoclastic varieties of Vendian-Early Cambrian rocks (b); (7) Vendian subalkalic basalt; (8) Vendian-Early Cambrian carbonaceous carbonate turbidite; (9) Vendian dolomitized calcarenite and calcilutite; (10) carbonate breccias of underwater slumping origin; (11) barite mineralization; (12) geologic boundaries and contacts between landslide slabs; (13) normal faults.


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