The C2 and C3 formations of the Schisto-Calcaire Subgroup (West Congo Supergroup) in the Democratic Republic of the Congo: An example of post-Marinoan sea-level fluctuations as a result of extensional tectonisms

Author:

Delpomdor F.,Tack L.,Cailteux J.,Préat A.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference155 articles.

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