Zobrazeno 1 - 10
of 34
pro vyhledávání: '"Katja Deckart"'
Publikováno v:
Minerals, Vol 11, Iss 8, p 903 (2021)
The oceanic seabed contains a variety of mineral resources related exclusively to submarine environments. Limited information has been documented for the seabed offshore of Chile, which is particularly interesting due to its geodynamic context and la
Externí odkaz:
https://doaj.org/article/799c6eaf40804ad7bd1bfa30f8047be2
Publikováno v:
Andean Geology, Vol 37, Iss 1, Pp 1-31 (2010)
Four Middle-to-Late Miocene barren plutonic complexes that occur between the giant porphyry copper deposits of the central Chilean Andes were selected for U-Pb LA-ICPMS geochronology and Hf-isotope systematics on single zircon grains. Major and trace
Externí odkaz:
https://doaj.org/article/a62857bc7765459d9c9185d139b236a8
Publikováno v:
Environmental Geochemistry and Health. 44:3173-3189
The importance of environmental geochemistry baseline in soils of O´Higgins Region, Chile, since it hosts in its eastern area one of the major Cu-Mo producing mines in the country, is to establish and explain relationships between the chemical compo
Publikováno v:
Gondwana Research. 76:303-321
The tectonic evolution of the southwestern margin of Pangea supercontinent is represented by the extensive late Paleozoic–Triassic magmatism along the southwestern margin of South America, including the Chilean Frontal Andes batholiths as part of t
Autor:
Ana Valdés Durán, Josefa Velásquez, Gloria Neculqueo, Katja Deckart, Dante Cáceres Lillo, Luis Navarro Frez, Danny Tröger, Alejandra Canales Quezada, Marx Buscaglia Solé, María Eliana Escobar
Publikováno v:
Journal of South American Earth Sciences. 118:103927
Autor:
César Arriagada, Katja Deckart, Juan Becerra, Andrei Maksymowicz, Fernando Martínez, Sebastián Bascuñán
Publikováno v:
Tectonophysics. 759:58-78
The late Mesozoic-Cenozoic evolution of the Central Andes of northern Chile consists of a series of events related to changing conditions along the plate margin, leading to different episodes of compression and extension. A long-lasting basin which r
Publikováno v:
Gondwana Research. 37:172-181
The Andean orogenic cycle and its subduction-related magmatism along the southwestern margin of South America began during the early Jurassic after an accretionary history throughout Paleozoic times. The Chilean and Argentinian Frontal Andes batholit
Publikováno v:
Tectonophysics. 667:144-162
The Andean orogenic belt, located in the Central Andes “Pampean flat-slab” segment in northern Chile (27–29°S), is composed of two major tectonic regions: the Coastal Cordillera and the Frontal Cordillera. To understand their internal tectonic
Publikováno v:
Journal of South American Earth Sciences. 64:307-324
The structure of the Chilean Frontal Cordillera, located over the Central Andes flat-slab subduction segment (27°–28.5°S), is characterized by a thick-skinned deformation, affecting both the pre-rift basement and the Mesozoic and Cenozoic infill
Autor:
Osvaldo Martínez, Katja Deckart, Ryan Mathur, Marcia Muñoz-Gómez, Brian Townley, Valentina Díaz
Publikováno v:
Ore Geology Reviews. 122:103522
The Brahma prospect is a Neogene porphyry copper deposit located in the Chilean Andes at ~ 35°45′S, beyond the southerly extension of the previously defined Mio-Pliocene metallogenic belt of Central Chile. We present the results of a comprehensive