Organic Geochemistry of Shale Outcrop From the Morro Do Chaves Formation, Lowercretaceous, Sergipe-Alagoas Basin, Northeastern Brazil
This study characterizes the organic geochemistry of shales from the Lower Cretaceous Morro do Chaves Formation in Brazil, revealing a complex lacustrine depositional environment with periodic marine incursions driven by tectonic and climatic oscillations during the Gondwana breakup.