Rogelio Daniel Acevedo Geological Records of the Fuegian Andes Deformed Complex Framed in a Patagonian Orogenic Belt Regional Context 9783030001650

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Автор: Rogelio Daniel Acevedo
Название: Geological Records of the Fuegian Andes Deformed Complex Framed in a Patagonian Orogenic Belt Regional Context
ISBN: 9783030001650
Издательство: Springer
Классификация:

Ботаника и науки о растениях

Геология и литосфера

Почвоведение, седиментология

Геологические поверхностные процессы (геоморфология)

ISBN-10: 3030001652
Обложка/Формат: Soft cover
Страницы: 113
Вес: 0.27 кг.
Дата издания: 2019
Серия: SpringerBriefs in Earth System Sciences
Язык: English
Издание: 1st ed. 2019
Иллюстрации: 48 illustrations, color; 15 illustrations, black and white; ix, 113 p. 63 illus., 48 illus. in color.
Размер: 235 x 155
Читательская аудитория: Professional & vocational
Основная тема: Earth Sciences
Ссылка на Издательство: Link
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Поставляется из: Германии
Описание: This book studies the Fuegian Andes in Argentina, showing both simple and complex aspects. The first ones refer to the general stratigraphy of the area and the latter result from their tectonic characteristics. Concerning the stratigraphy, an appraisal of the denomination and valorization of formations of Jurassic and early Cretaceous age is performed here to reach the simple scheme of the Fuegian-Patagonian continuity under the name of “Fuegian Andes Deformed Complex”. As an essay the formational nomenclature is simplified and the local concept of basement 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 early Tertiary layers are connected phenomena. Tectonic forces from the West, the Northeast and the South have had participation in the formation of the tectonic arc. The lithostatic column pressure was added once the layers were folded and thrusted upwards during the birth of the Fuegian Andes. Even the speculation of a great main fold overturned to North, as an abstraction, is considered. Instead, the Magallanes-Fagnano fault is appreciated only as a product of the transcurrent Quaternary movements, lacking associated eruptive processes that contribute to define plate borders.
Дополнительное описание: 1:Introduction.- 2:Background.- 3:The geological formations of the Mesozoic complex.- 4:The basic eruptive rocks of the Alvear and Sorondo ranges (Mount Olivia).- 5:The Cretaceous layers younger than the Early Cretaceous.- 6:The estimated basement for the

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