Zobrazeno 1 - 8
of 8
pro vyhledávání: '"VEX 100"'
Autor:
Bachmann, Raik
Publikováno v:
Scientific Technical Report STR
Title, Contents, Summary, Zusammenfassung 1\. Introduction 1 1.1. Overview 1 1.2. Objectives and motivation 2 1.3. Working areas 2 1.3.1. Alps 2 1.3.2. Chile 7 2\. Methods 13 2.1. Overview 13 2.2. Analyses of structural data 13 2.3. PT estimates 13 2
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2a2cccaa8b4392f5cd9e462a16db72fd
http://hdl.handle.net/11858/00-1735-0000-0001-32B7-D
http://hdl.handle.net/11858/00-1735-0000-0001-32B7-D
Autor:
Melnick, Daniel
The Andean orogen is the most outstanding example of mountain building caused by the subduction of oceanic below continental lithosphere. The Andes formed by the subduction of the Nazca and Antarctic oceanic plates under the South American continent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2a83f113f2393dbbf39d2ba784d1aaef
http://hdl.handle.net/11858/00-1735-0000-0001-31D5-2
http://hdl.handle.net/11858/00-1735-0000-0001-31D5-2
Autor:
Elger, Kirsten
The Altiplano represents a key region of the Central Andes, where the interplay between faults and syn-tectonic sediments allow the reconstruction of the kinematic evolution of the Central Andean high plateau. This study aims, by the use of increment
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1ba1552f3ced26a844a33e94d9824a38
http://doi.org/10.2312/GFZ.B103-03052
http://doi.org/10.2312/GFZ.B103-03052
Autor:
Muñoz, Alberto Adriasola
Fission track (FT) thermochronology of zircon and apatite combined with structural analyses on deformed rocks was applied to investigate the cooling and denudation history of the Southern Chilean Andes at 41ʿ-42ʿS in relation to the late Cenozoic a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a332ba1f074a7313634df90c0c26e236
http://hdl.handle.net/11858/00-1735-0000-0001-3207-8
http://hdl.handle.net/11858/00-1735-0000-0001-3207-8