
																
																	Hydrothermal alteration related to a deep mantle source controlled by a Cambrian intracontinental strike-slip fault: Evidence for the Meruoca felsic intrusion associated with the Transbraziliano Lineament, Northeastern Brazil
																
																
																
															Keywords: ایزوتوپهای پایدار; Transbraziliano Lineament; Granitic intrusion; Hydrothermal alteration; Stable isotopes