The Southern Central Andes: Contributions to Structure and Evolution of an Active Continental Margin: Lecture Notes in Earth Sciences, cartea 17
Editat de Heinrich Bahlburg, Christian Breitkreuz, Peter Gieseen Limba Engleză Paperback – 27 iul 1988
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Specificații
ISBN-13: 9783540500322
ISBN-10: 3540500324
Pagini: 272
Ilustrații: VIII, 261 p. 77 illus.
Dimensiuni: 170 x 244 x 14 mm
Greutate: 0.44 kg
Editura: Springer Berlin, Heidelberg
Colecția Springer
Seria Lecture Notes in Earth Sciences
Locul publicării:Berlin, Heidelberg, Germany
ISBN-10: 3540500324
Pagini: 272
Ilustrații: VIII, 261 p. 77 illus.
Dimensiuni: 170 x 244 x 14 mm
Greutate: 0.44 kg
Editura: Springer Berlin, Heidelberg
Colecția Springer
Seria Lecture Notes in Earth Sciences
Locul publicării:Berlin, Heidelberg, Germany
Public țintă
ResearchCuprins
Ancient crystalline basement provinces in the north chilean central andes — relics of continental crust development since the mid proterozoic.- The puncoviscana formation (late precambrian — early cambrian). - sedimentology, tectonometamorphic history and age of the oldest rocks of nw argentina.- Geology and sedimentology of the cambrian grupo meson (NW argentina).- Lower ordovician in the southern part of the argentine eastern cordillera.- Geology of the coquena formation (arenigian-llanvirnian) in the nw argentine puna: Constraints on geodynamic interpretation.- The paleozoic evolution of Northern Chile: Geotectonic implications.- Marine mesozoic paleogeography in Northern Chile between 21°–26°S.- Tectonic framework and correlations of the cretaceous-ecocene salta group; Argentina.- The cenozoic saline deposits of the chilean andes between 18°00? and 27°00? south latitude.- Geomorphological west-east-section through the north chilean andes near antofagasta.- The jurassic la negra formation in the area of antofagasta, Northern Chile (lithology, petrography, geochemistry).- Cenozoic ignimbrites of the central andes: A new genetic model.- Central andean gravity field and its relation to crustal structures.- Seismicity and crustal structure of the central andes.- Structures and crustal development of the central andes between 21° and 25°S.