Victor A. Ramos – författare

The science of geology is intertwined with the growth of the field in Argentina. This book explores those dual historical developments and, as an expanded translation of Historia de la Geología Argentina: Una Crónica de Más de Dos Siglos, shares them with a global audience. Drawing on the author's extensive work throughout the country as well as documents and photographs from the archives of the National Geological Survey, General Archive of the Nation, and the universities of Buenos Aires, Córdoba, and La Plata, this book offers a once-in-a-century look at developments in the field of geology from a country-specific perspective.

The science of geology is intertwined with the growth of the field in Argentina. This book explores those dual historical developments and, as an expanded translation of Historia de la Geología Argentina: Una Crónica de Más de Dos Siglos, shares them with a global audience. Drawing on the author's extensive work throughout the country as well as documents and photographs from the archives of the National Geological Survey, General Archive of the Nation, and the universities of Buenos Aires, Córdoba, and La Plata, this book offers a once-in-a-century look at developments in the field of geology from a country-specific perspective.

Convergent plate margins and subduction zones are first order features shaping the Earth. Convergent continental margins combine the majority of processes that affect the internal architecture thermal and geochemical character of continental lith- phere. In addition, the close relationships between active deformation and uplift, m- matism and associated crustal growth, ore formation, the release of more than 90% of global seismic energy at convergent margins, make these plate boundaries imp- tant natural laboratories where mass and energy flux rates can be studied at various scales. Since the advent of plate tectonic theory, it has been recognized that all of these phenomena are intimately related and often governed by feedback mechanisms. Accordingly, subduction orogeny has become an international, high-priority theme in process-oriented, earth-system analysis. In this context, Dewey and Bird (1970) have defined the Andes as the type representative for orogeny and associated p- cessesat convergent margins in their benchmark paper. The Andes, therefore, p- vide an excellent natural laboratory for studying the above processes.

Convergent plate margins and subduction zones are first order features shaping the Earth. Convergent continental margins combine the majority of processes that affect the internal architecture thermal and geochemical character of continental lith- phere. In addition, the close relationships between active deformation and uplift, m- matism and associated crustal growth, ore formation, the release of more than 90% of global seismic energy at convergent margins, make these plate boundaries imp- tant natural laboratories where mass and energy flux rates can be studied at various scales. Since the advent of plate tectonic theory, it has been recognized that all of these phenomena are intimately related and often governed by feedback mechanisms. Accordingly, subduction orogeny has become an international, high-priority theme in process-oriented, earth-system analysis. In this context, Dewey and Bird (1970) have defined the Andes as the type representative for orogeny and associated p- cessesat convergent margins in their benchmark paper. The Andes, therefore, p- vide an excellent natural laboratory for studying the above processes.