Petrogenesis and geodynamic setting of Ediacaran rocks from the Sirwa massif, Central Anti-Atlas of Morocco
The geodynamic evolution of the post-Pan-African Anti-Atlas Orogeny (∼ 650 Ma) remains debated, particularly regarding the basement beneath the Central Anti-Atlas and the geological processes leading to the formation of the Ediacaran Saghro Group (SG) and Ouarzazate Group (OG). New LA-ICP-MS U-Pb ages of 575 ± 3 Ma a...