2021
DOI: 10.1007/s41513-020-00154-9
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Ophiolitic rocks and plagiorhyolites from SW Ecuador (Cerro San José): petrology, geochemistry and tectonic setting

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Cited by 4 publications
(2 citation statements)
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“…Regionally, Ecuador is divided into tectonostratigraphic zones that extend parallel to the Northern Andes mountain range. From west to east, these are: (1) the oceanic terranes of the coastal region and the Late-Cretaceous Western Cordillera [61][62][63][64]. (2) the Chingual-Cosanga-Pallatanga-Puná (CCPP) dynamic fault system [65], which is also the eastern tectonic limit of the "North Andean Sliver" and is related to the oblique subduction of the Nazca plate.…”
Section: Geological Settingmentioning
confidence: 99%
“…Regionally, Ecuador is divided into tectonostratigraphic zones that extend parallel to the Northern Andes mountain range. From west to east, these are: (1) the oceanic terranes of the coastal region and the Late-Cretaceous Western Cordillera [61][62][63][64]. (2) the Chingual-Cosanga-Pallatanga-Puná (CCPP) dynamic fault system [65], which is also the eastern tectonic limit of the "North Andean Sliver" and is related to the oblique subduction of the Nazca plate.…”
Section: Geological Settingmentioning
confidence: 99%
“…From a geological point of view, the study area soil is composed of volcanic materials (Piñón Formation) and sedimentary volcano materials (Cayo Formation). On top of these materials there are cretaceous and tertiary sedimentary materials [35][36][37][38][39]. The study area's relief is made up of plains and undulating hills, with medium to gentle slope [40].…”
Section: Study Areamentioning
confidence: 99%