3 edition of Nappe theory in the Alps (Alpine tectonics, 1905-1928) found in the catalog.
Nappe theory in the Alps (Alpine tectonics, 1905-1928)
Translation of : Die Deckentheorie in den Alpen.
|Statement||by Franz Heritsch ; translated by P.G.H. Boswell.|
|Series||Methuen"s geological series|
|The Physical Object|
|Pagination||xxx,228p.,7leaves of plates|
|Number of Pages||228|
The tectonic evolution of the Alpine belt in Crete was created by north-dipping, Miocene-Cretaceous subduction between Apulia and a Gondwana-derived microcontinent called Mesogea with Europe (Creutzburg and Seidel, ; Le Pichon and Angelier, ; Seidel et al., ; Bonneau, ; Hall et al., ).South-vergent nappes, which moved along north-dipping thrusts partially along underlying Cited by: When Manfred Gwinner dared to write a book summarizing the geology of the Alps for the uninitiated, the ﬁrst sentence in his preface (of both editions: , ) was a south-vergent slices in front and atop the Suretta Nappe is, in my view, worth The geosynclinal theory of mountain build-.
Criticism of the systems put forward by the Comitato Geografico Nazionale Italiano and by prof. de Martonne in his recent book on the Alps. L. KOBER, Bau und Entstehung der Alpen, Berlin ; Ch. KNAPP et M. BOREL, Dictionnaire Géographique de la Suisse, Neuchâtel ;. The nappe theory developed in the Western Alps, but was soon exported to the Eastern Alps, and then to the rest of the globe, by the Swiss geologist Emile Argand ( - ), who between to draw the first profile of the Penninic zone and then represented the structural setting of the entire Western Alps in a , tectonic map and corresponding cross-sections.
The theory of plate tectonics was one of the great scienti ic revolutions of the twentieth century and is fundamental to our understanding of how mountain ranges like the Alps are built. Buy The High Mountains of the Alps by Dumler, Helmut (ISBN: ) from Amazon's Book Store. Everyday low prices and free delivery on eligible orders/5(4).
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Additional Physical Format: Online version: Heritsch, Franz, Nappe theory in the Alps. London, Methuen  (OCoLC) Document Type. The nappe theory in the Alps: (Alpine tectonics, ) (Methuen's geological series) [Heritsch, Franz] on *FREE* shipping on qualifying offers.
The nappe theory in the Alps: (Alpine tectonics, ) (Methuen's geological series)Author: Franz Heritsch. Franz Heritsch (26 December in Graz – 17 April in Graz) was an Austrian geologist and paleontologist, known for his studies of the Paleozoic of the Eastern Alps.
From to he studied at the University of Graz, and following graduation, worked as a middle school teacher in he obtained his habilitation, and later on, served as an associate (–24), and full Authority control: GND:ISNI:. The English word Alps derives from the Latin Alpes (through French).Maurus Servius Honoratus, an ancient commentator of Virgil, says in his commentary (A.
X 13) that all high mountains are called Alpes by Celts. The term may be common to Italo-Celtic, because the Celtic languages have terms for high mountains derived from alp.
This may be consistent with the theory that in Coordinates: 45°49′58″N 06°51′54″E / °N. The Nappe Theory in the Alps (Alpine Tectonics, - ) Heritsch, Dr. Franz, Translated By P.
Boswell. Open Library is an open, editable library catalog, building towards a web page for every book ever published.
Author of The Nappe theory in the Alps (Alpine tectonics, ), Die deckentheorie in den Alpen. A NDJ. ': A stable and 40Ar/39Ar isotope study of a major thrusi in the Helvetic nappes (SwÎ5s Alps): Evidence for fluid constraints on nappe kinematics, Bull, GeaL Soc. The Alps, with their outstanding outcrop conditions, represent a superb natural laboratory for many geological processes, Nappe theory in the Alps book 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. of the Helvetic nappe system, the true birth date of the nappe concept in the Alps, according to Trümpy (), is the publica- tion by Schardt.
The nappe theory in the Connecticut Valley region: Thirty-five years since Jim Thompson's first proposal INrnonucltotl a paraphrase from the book, The Nappe Theory in the We discuss an area in the central New England Appa- l/ps (Heritsch, ). in which Zone in the European Alps. This theory began with.
CHAPTER EIGHT The Nappe Theory in the Alps: Tectonics over Physics, – (pp. ) That Eduard Suess should have gained an immediate international following for a theory unlike any of its predecessors in a science notable for the acrimony of its controversies was the result of a.
Heritsch, Franz Overview. Works: The nappe theory in the Alps (Alpine tectonics, ) by Franz Heritsch (Book) 14 editions published. 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/5(6). The Nappe Theory in the Alps: Tectonics over Physics, THAT Eduard Suess should have gained an immediate international following for a theory unlike any of its predecessors in a science notable for the acrimony of its controversies was the result of a complex accident.
Suess was a great geologist and a manCited by: The English word Alps derives from the Latin Alpes (through French).
Maurus Servius Honoratus, an ancient commentator of Virgil, says in his commentary (A. X 13) that all high mountains are called Alpes by term may be common to Italo-Celtic, because the Celtic languages have terms for high mountains derived from alp.
This may be consistent with the theory that in Greek Alpes is a. The nappe theory was established and again progressed in the Western Alps, reaching world-wide dimension thanks to the genius of Emile Argand (71, 37, 25).
4, 5, 6 first reconstructed the metamorphic nappes of the Penninic zone and then represented the structural setting of the entire Western Alps in atectonic map and by: In Gagnebin earned the licence in natural and physical sciences and became assistant to Maurice Lugeon, a specialist in the tectonics of Switzerland and one of the first advocates of the nappe theory of the Alps.
He began geological researches toward his doctorate in ; they dealt with the Préalpes Bordières and the region of Ch. Seen at first as evidence of von Buch’s theory of magmatic rocks uplifting sedimentary layers, nowadays it is seen as a example of the Alpine nappe structure.
Here partial erosion removed part of the nappe, forming a tectonic window, where the oldest rocks found in the Alps remerge to the surface. Tectonophysics, () Eisevier Science Publishers B.V., Amsterdam Formation of Alpine mylonites and pseudotachylytes at the base of the Silvretta nappe, Eastern Alps Norbert Koch and Ludwig Masch Mineralogisch-Petrographisches Institut der Universit Mchen, Theresienstra D Munich 2, Germany (Received January 9,; accepted Ma) ABSTRACT Koch, N.
Cited by: Émile Argand was a Swiss geologist who is noted for developing the theory of embryotectonics, which was the idea that prehistoric ridges and valleys guide the growth of fold mountains.
He is also regarded as a specialist in tectonics, who was among the first to understand nappes (rocks sheets that are pressed to move sideways), explaining the complex structure of the Pennine and Western Alps. The Lyngen Magmatic Complex itself sits on top of another nappe - the Reisa Nappe Complex.
research has mapped three of the Lyngen units and shows a more complex differentiation of rocks than a single massive area of gabbro (see Oliver, G.J.H. and Krogh, T.E., () U-Pb zircon age of + 5 Ma for a metatonalite from the Kjosen Unit of.Books set in French Alps: [Point Blank, The Reunion, Paws of the Yeti, Chalet Boy - The Diary of My First Ski Season] Rate this book.
Clear rating. 1 of 5 stars 2 of 5 stars 3 of 5 stars 4 of 5 stars 5 of 5 stars. Paws of the Yeti (Blue Moon Investigations #9) by. Steve Higgs (Goodreads .The Alps extend in an arc from France in the south and west to Slovenia in the east, and from Monaco in the south to Germany in the north.
The Alps are a crescent shaped geographic feature of central Europe that ranges in an km ( mi) arc (straight line) from east to west and is km ( mi) in width.
The mean height of the mountain peaks is km ( mi). .