Tracing large-scale MTD architecture at basin margins: from protolith to MTD

VICTORIA VALDEZ BUSO Y JUAN PABLO MILANA

San Juan

Simposio; Slopes Consortium Final Meeting; 2012

University of Aberdeen

CONCLUSIONS: A) SIERRA DE MAZ´MTD 2 IS THE SAME AS MTD2 IN CERRO BOLA, BUT IN MAZ IT LAPS ON TO THE MARGIN BASIN. B)WE CAN SEE THE MATERIAL IN PLACE AND THE TRANSITION FROM UNDEFORMED PROTOLITH TO DEFORMED MTD. C)THE MTD EXTENSION IS c.15 KM FROM SA DE MAZ TO CERRO BOLA D) IN MAZ THERE IS GOOD RELIEF ON TOP OF MTD SURFACE AND PONDING. E)LARGE DOWNCUTTING OF STRATIGRAPHY IN MAZ ALONG EARLY POSTDEPOSITIONAL FAULTS.