Cenozoic Volcanism in the Mediterranean Area 1-1-001-323-4330-323 Lake Creede was a late

Lake Creede was a late Oligocene closed-basin lake that existed in the moat of the Creede caldera in the central San Juan Mountains

melt segregation

and a review of tectonic models for the Limpopo Complex

five articles in the alternatives section argue against existence of the megashear as originally proposed and provide alternative interpretations to explain geologic relations in northern Mexico and the southwestern United States

and philosophical questions in the evolution of geological thought

Cenozoic Volcanism in the Mediterranean Area 1-1-001-323-4330-323 Lake Creede was a lateEditors: Luigi Beccaluva, Gianluca Bianchini, and Marjorie Wilson The widespread volcanism that affected the Mediterranean region during the Cenozoic includes a wide spectrum of magmatic affinities reflecting the complex geodynamic setting of the area. Magmatism is linked to the evolution of a series of subduction zones formed during Africa Eurasia convergence, including the relative migration of trench arc systems, opening of interarc basins, and the