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The plutonic rocks of the westernmost part of the Sirwa massif belong to the Ediacaran post-collisional magmatic chain of the Anti-Atlas.The geochemistry of major and trace elements attests that the fractional crystallization cannot account for the variations between the granitoids and the associated MME.They represent two contemporaneous but independent magmatic tendencies.However,Sr and Nd configur data argue for a similar and juvenile material source
The plutonic rocks of the westernmost part of the Sirwa massif belong to the Ediacaran post-collisional magmatic chain of the Anti-Atlas. The geochemistry of major and trace elements attests that the fractional crystallization can not account for the variations between the granitoids and the associated MME They represent two contemporaneous but independent magmatic tendencies. However, Sr and Nd configur data argue for a similar and juvenile material source