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2 edition of Geological framework of the Western Alps found in the catalog.

Geological framework of the Western Alps

I.G.C.P. 235 Excursion to the Alps. (1988 Turin-Genoa).

Geological framework of the Western Alps

field meeting on highecologitic reequilibrium in the Western Alps

by I.G.C.P. 235 Excursion to the Alps. (1988 Turin-Genoa).

  • 235 Want to read
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Published by [IGCP Project 235] in [Genoa] .
Written in English


Edition Notes

Other titlesHigh pressure eclogitical reequilibrium in the Western Alps.
Statementedited by G.B. Piccardo.
ContributionsPiccardo, G. B., International Geological Correlation Programme. Project 235 - Metamorphism and geodynamics.
ID Numbers
Open LibraryOL14306269M

Try the new Google Books. Check out the new look and enjoy easier access to your favorite features. Try it now. Authorities to be consulted on the Geology of the Alps. cxxiv: List of Works on the Alps cxx V. cxxxiii: A Guide to the Western Alps Part 1 of Arupain gaido Part 1 of The Alpine guide: Authors: John Ball, Édouard Desor.   If you would like to find out more about the geology of the Alps, an excellent resource is the book ‘The Alps and our Planet, The African Matterhorn: A Geological Story’ by Michel Marthaler. If you are interested in seeing the magnificent geology of the Alps firsthand, you may want to consider a trekking tour of the Alps.

Only at the western end of the Pennine Alps, another nappe is sandwiched between Siviez-Mischabel Nappe and Zone Houillière Nappe: the Ruitor Zone, formed by Variscan basement rocks. In an early stage, the partial nappes of the d Nappe were recumbent folds with a basement core and normal as well as inverted limbs of Mesozoic cover. Regional geology is the geological study of large-scale regions. Usually, it encompasses multiple geological disciplines to piece together the history of an area. It is the geologic equivalent of regional size and the borders of each region are defined by geologically significant boundaries and by the occurrence of geologic processes.

Reconstructions of the Tethyan realm have been a matter of debate for a long time. Controversies spring usually from a lack of well constrained geological data which can be interpreted in different ways, or, from a lack of constraints on the plate tectonics framework. The western Alps region tends to escape these shortcomings due to a wealth of geological data regarding for examples the. zone (Figure 1), which crosses the Alps in an oblique direction. This shear zone is intimately linked to the transition of the central to the western Alps and the formation of the Western Alpine arc, which is the main topic of the present contribution. 2. Tectonic Reinterpretation of the ECORS- CROP Profile of the Western Alps


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Geological framework of the Western Alps by I.G.C.P. 235 Excursion to the Alps. (1988 Turin-Genoa). Download PDF EPUB FB2

The present structural framework of the western Alps is shown in figures 1 and 2 (modified from Marchant, ; Marchant and Stampfli, a; Marchant and Stampfli, b), and are based on a structural model developed mainly by the Lausanne school (e.g Escher et al., ; Escher et al., ; Steck et al., ; Steck et al., ).

Geology of the Western Swiss Alps: A Guide-book Issue 36 of Mémoires de Geologie, ISSN Volume 36 of Mémoires de géologie, Lausanne: mémoires des Laboratoires de géologie, minéralogie, géophysique et du Musée géologique de l'Université de Lausanne Issue 36 of Mémoires de géologie, Lausanne, ISSN The Alps have a complex geology, but the general structure is the same as for other mountain ranges formed by continental collision.

Subdivisions [ edit ] The Alps are often divided into Eastern, Central and Western Alps, even though the boundaries between these subdivisions are arbitrary. The book goes on to describe the structure of the Alps (including the Jura Mountains and the Alpine foreland to the north and south) illustrated by numerous cross-sections.

Understanding the Author: O. Adrian Pfiffner. Therefore, the Western Alps and surrounding regions represent a key-stone for the western Tethys reconstruction. A detail account of the geological evolution along a western Swiss Alps transect is.

The book goes on to describe the structure of the Alps (including the Jura Mountains and the Alpine foreland to the north and south) illustrated by numerous cross-sections. The evolution of the Alps as a mountain chain incorporates a discussion of the Alpine metamorphic history and a compilation of orogenic timetables.

Our model is consistent with the commonly accepted paleogeography of the western Alps, wherein the locus of the oceanic suture is given by the present structural position of the oceanic units. The precollisional setting that we propose for the western Alps is comparable to the tectonic configuration around the Gulf of Oman, where continent.

Structural and geomorphological framework of the upper Maira Valley (Western Alps, Italy): the case study of the Gollone Landslide.

Journal of Maps: Vol. 16, No. 2, pp. The first discovery of ultrahigh-pressure coesite in the European Alps 30 years ago led to the inference that a positively buoyant continental crust can be subducted to mantle depth; this had been considered impossible since the advent of the plate tectonics concepts.

The geodynamic framework of the western Alps The plate tectonics of the western Tethyan regions The reconstructions shown in figure 4 to 9 are based on a tight pre break-up Permian fit (fig 3) as well as magnetic anomalies from the Central Atlantic.

The Alps, with their outstanding outcrop conditions, represent a superb natural laboratory for many geological processes, and have played a crucial role in the history of geology.

This book gives an up-to-date and holistic overview of the key aspects of Alpine geology. After a brief presentation of the plate tectonic framework, the rock suites are discussed, starting with the pre-Triassic. Home» Geology Of The Alps» Geology Of The Alps Book» Geology Of The Alps Pdf» Geology Of The Alps Download Free.

By Ethelene Reinhart Sabtu, 21 A Simplified Geologic Map Of The Western European The Alps Ppt Video Online Download Controlling Factors For Deep Seated Gravitational Slope. A new interpretative crustal‐scale section across the south‐western Alps is proposed, combining geological and geophysical 2D/3D data.

The Apulian mantle (i.e. the Ivrea body) might be divided into two rigid pieces separated by the downward prolongation of the Penninic frontal thrust. Marco G. Malusà, Paul G. Fitzgerald, The geologic interpretation of the detrital thermochronology record within a stratigraphic framework, with examples from the European Alps, Taiwan and the Himalayas, Earth-Science Reviews, /rev, (), ().

The Alps, with their outstanding outcrop conditions, represent a superb natural laboratory for many geological processes, and have played a crucial role in the history of geology.

Geology of the Alps gives an up-to-date and holistic overview of the key aspects of Alpine geology. After a brief presentation of the plate tectonic framework, the.

The regional geology of France is commonly divided into the Paris Basin, the Armorican Massif, the Massif Central, the Aquitaine Basin, the Pyrenees, the Alps, the Côte languedocienne, the Sillon rhodanien, the Massif des Vosges, the Massif Ardennais, the.

The book goes on to describe the structure of the Alps (including the Jura Mountains and the Alpine foreland to the north and south) illustrated by numerous cross-sections. The evolution of the Alps as a mountain chain incorporates a discussion of the Alpine metamorphic history and a compilation of orogenic s: 6.

This book gives an up-to-date and holistic overview of the key aspects of Alpine geology. After a brief presentation of the plate tectonic framework, the rock suites are discussed, starting with the pre-Triassic crystalline basement, followed by Paleozoic, Mesozoic and Reviews: 1.

Controversies spring usually from a lack of well constrained geological data which can be interpreted in different ways, or, from a lack of constraints on the plate tectonics framework.

The western Alps region tends to escape these shortcomings due to a wealth of geological data regarding for examples the rifting and spreading of the Alpine. Lecture notes by Nikolaus Froitzheim. Deutsche Version. PDF version (~3MB) Chapter 1: Introduction The Alps are, in a geological sense, a collisional orogen resulting from the collision of the European continent (“Europe”) with the Adriatic continent (“Adria”, also termed “Apulia”) after the subduction of intervening ocean basins.

The collision took place in the Tertiary but was. The Western Alps, from Rift to Passive Margin to Orogenic Belt addresses the evolution of the Alpine fold belt for the first time in the English language.

It builds on classical Alpine geological studies made since the start of the 19th century by combining that research with modern results obtained over the past 50 years using new marine geological and geophysical technologies.The Alps, with their outstanding outcrop conditions, represent a superb natural laboratory for many geological processes, and have played a crucial role in the history of geology.

This book gives an up-to-date and holistic overview of the key aspects of Alpine geology.Geology of the western Swiss Alps, a guide-book. Stampfli G.M. This guide book presents 6 field trips divided in two sections corresponding to the Alpine Externides and Internides, of the western Swiss Alps.

A good share of basement geology is included in the guide, and two field trips (Ft1 and Ft5) are mainly devoted to Variscan and.