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The Western Alps, from Rift to Passive Margin to Orogenic Belt

The Western Alps, from Rift to Passive Margin to Orogenic Belt addressesthe evolution of the Alpine fold beltfor the first time;

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Permo-Triassic Salt Provinces of Europe, North Africa and the Atlantic Margins

western and northern Tethys (from Iberia and North Africa, Pyrenees and Alps, Adriatic and Ionian) during the subsequent Alpine orogenic processes;

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Growth of the Southern Andes

, it illustrates the diversity of mechanisms that have impacted strong orogenic gradients and consequently mountain morphology, from the;

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Middle American Terranes, Potential Correlatives, and Orogenic Processes

from flat-slab subduction related to overriding a plume; and (3) Mesozoic-Cenozoic events along the western margin of Laurentia * A;

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Understanding an Orogenic Belt

The book provides a model for the structural evolution of the Himalaya with relevant background information making it easily accessible to;

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Formation and Crust-Mantle Geodynamic Processes of the Neoarchean K-rich Granitoid Belt in the Southern Range of Eastern Hebei-Western Liaoning Provinces, North China Craton

mechanisms, during which the average composition of continental crust gradually shifted from Na-enriched to K-enriched. However, the ultimate source;

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In Sight of the Suture

interest to research workers in the geology of the Caledonian/Appalachian orogenic belt, to sedimentologists interested in deep marine processes;

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Orogenic Type Polymetallic Mineralization Associated with Multistage Orogenesis

metals took place as responses to orogenesis and metamorphism, leading to metal redistribution and the formation of orogenic-type orebodies. The;

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Geology of the Alps

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;

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Geology of the Alps

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;

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The Ross Orogen of the Transantarctic Mountains

-day Antarctica. According to a recent hypothesis, this continental margin was created by the rifting and subsequent drift of Laurentia from;

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Orogenesis: The Making Of Mountains

belts such as the Alps or Himalayas or causing one plate to be subducted below the other, resulting in volcanic mountain chains such as the;

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A Guide to the Western Alps

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The Great Rift Valleys of Pangea in Eastern North America

rift province, collectively called the central Atlantic margin system, spans more than 45 degrees of paleolatitude and records over 35 million;

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A dynamic stratigraphy of the British Isles

Caledonian and Hercynian orogenic cycles, to the evolution of NW Europe on the margin of the opening Atlantic Ocean. A full synthesis of geological;

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The Great Rift Valleys of Pangea in Eastern North America

rift province, collectively called the central Atlantic margin system, spans more than 45 degrees of paleolatitude and records over 35 million;

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Tectonics of Sedimentary Basins

leading researchers in this field have been brought together in this volume to provide concise overviews of the current state of the subject. The;

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Storming the Eagle's Nest

From the Fall of France in June 1940 to Hitler's suicide in April 1945, the swastika flew from the peaks of the High Savoy in the western;

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Orogenic Processes in the Alpine Collision Zone

very up-to-date review and research articles covering the Alps, Carpathians and Dinarides. These data were presented at the 8th workshop on;

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Source and Sediment

reconstructable from its erosional products released to the sea; from gravel and sand, from silt, sand, clay which recombine to form a new cycle of rocks;

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Continental Margin Sedimentation

This volume on continental margin sedimentation brings together an expert editorial and contributor team to create a state-of-the-art;

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The Geology of the Belingwe Greenstone Belt, Zimbabwe

A study on the Bellingwe Greenstone Belt, presenting the stratigraphy of the belt, its structure and tectonic setting, the sedimentology;

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Tundras

western Italian Alps. In addition, treeline ecotone is a belt of transition from forest vegetation to a non-forest one, which allow the monitoring;

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Geological Records of the Fuegian Andes Deformed Complex Framed in a Patagonian Orogenic Belt Regional Context

is evaluated. In relation to their structural aspects it is assumed that the formation of the orogenic Fuegian arc and the folding of the Mesozoic and;

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Tectonics of Asia (Northern, Central and Eastern Asia)

structures of Asia. The final chapter of the book describes the tectonic evolution of the Central Asian Orogenic Belt from the Neoproterozoic to the;

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Tectonic Evolution of the Tethyan Region

workers of this immense orogenic belt. Much new work had been completed in such previously little-known areas as Turkey, Iran, Afghanistan, the;

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Climate sensitivity of European larch in the French Maritime Alps

Mediterranean margin, these larches are able to reach an age of up to 1000 years probably belonging to the oldest larches of Europe. They are situated;

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