Geodynamics Of The Alps 1

Geodynamics of the Alps consists of three volumes. This first volume describes the recent and present-day structure and tectonic setting of the Alpine chain, from the lithospheric mantle to brittle crust and surface topography. It also provides a historical overview of Alpine research, with two chapters covering specific Alpine regions (Corsica and the Eastern Alps) through all phases of Alpine history. The aim of this book is to create a space for experts on Alpine research to present the state of the art of specific subjects and provide their own interpretations.

Geodynamics of the Alps consists of three volumes. This first volume describes the recent and present-day structure and tectonic setting of the Alpine chain, from the lithospheric mantle to brittle crust and surface topography. It also provides a historical overview of Alpine research, with two chapters covering specific Alpine regions (Corsica and the Eastern Alps) through all phases of Alpine history. The aim of this book is to create a space for experts on Alpine research to present the state of the art of specific subjects and provide their own interpretations.

Geodynamics of the Alps consists of three volumes. This third volume is entirely dedicated to Alpine collision. It describes and interprets elements of the Alpine chain, including Alpine magmatism, the formation of external massifs, the foreland basin, the exhumation of the internal part of the chain and the northern deformation front of the Alps. The aim of this book is to create a space for experts on Alpine research to present the state of the art of specific subjects and provide their own interpretations.

Geodynamics of the Alps consists of three volumes. This second volume presents the pre-collisional history of the Alps. It discusses the Variscan orogeny in the Alpine realm, the inferred paleo-geography, the structure and processes affecting continental margins and the mantle structure in the pre-orogenic Alpine realm. It concludes by describing oceanic and continental subduction processes. The aim of this book is to create a space for experts on Alpine research to present the state of the art of specific subjects and provide their own interpretations.

The objective of the National Research Program 20 (NRP 20), funded by the Chapter 7 covers three study areas in the Jura Mountains. In section 7. 1 a Swiss National Science Foundation, was to explore the deep structure of the reinterpretation of industry lines shed new light on the internal structure of Swiss Alps combining geophysical and geological methods. The data were the Folded Jura of the Neuchatel area. Here the role of thrust faults underly collected between 1986 and 1993. Processing and interpretation of the data ing major anticlines had previously been underestimated. Some of the folds involved over 50 researchers from Swiss universities and from industry. The could be interpreted as fault-propagation folds, with a detachment in the aim of this Atlas is to draw all this work together into a coherent compilation Muschelkalk evaporites. Section 7. 2 discusses the Tabular Jura around Basel. of the geological and geophysical data, their interpretation and integration A seismic line through this Basel Jura images the Moho on the southern flank into the tectonic evolution of the Swiss Alps. This turned out to be a difficult of the Black Forest-Vosges basement uplifts and suggests the presence of task. Late Paleozoic troughs underneath the Tabular Jura.

The objective of the National Research Program 20 (NRP 20), funded by the Chapter 7 covers three study areas in the Jura Mountains. In section 7. 1 a Swiss National Science Foundation, was to explore the deep structure of the reinterpretation of industry lines shed new light on the internal structure of Swiss Alps combining geophysical and geological methods. The data were the Folded Jura of the Neuchatel area. Here the role of thrust faults underly collected between 1986 and 1993. Processing and interpretation of the data ing major anticlines had previously been underestimated. Some of the folds involved over 50 researchers from Swiss universities and from industry. The could be interpreted as fault-propagation folds, with a detachment in the aim of this Atlas is to draw all this work together into a coherent compilation Muschelkalk evaporites. Section 7. 2 discusses the Tabular Jura around Basel. of the geological and geophysical data, their interpretation and integration A seismic line through this Basel Jura images the Moho on the southern flank into the tectonic evolution of the Swiss Alps. This turned out to be a difficult of the Black Forest-Vosges basement uplifts and suggests the presence of task. Late Paleozoic troughs underneath the Tabular Jura.