Γεωτεκτονική εξέλιξη των Άνδεων και σύγκριση με την εξέλιξη του ελληνικού ορογενούς = Geotectonic evolution of thw Andes and comparison to the evolution of thw Hellenic oregen.
Περίληψη
The Andes Mountains are one of the most important mountain ranges on Earth. It dominates the western coast of South America and is of particular interest, as it has a long history of evolution from the Paleozoic to the present day, with the active subduction of the Nazca oceanic plate beneath the continental fragment of South America. It presents a complex structure with different characteristics of its individual parts, and is therefore distinguished in northern, central and southern part. A complex tectonic history that led to an impressive elevation and the creation of plateaus, plays a key role in the evolution of the Andes, even in the climatic conditions of the wider region, as it is an important high "dam" between the two oceans, the Pacific and the Atlantic. Apart from basic elements in stages of the geotectonic cycle, the Hellenic orogeny and the orogeny of Andes, do not show similarities in their evolution.
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Ελληνική Βιβλιογραφία
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Διαδικτυακές Πηγές
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