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Gas origin linked to paleo BSR.
- Published in:
- Scientific Reports, 2021, v. 11, n. 1, p. 1, doi. 10.1038/s41598-021-03371-z
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A cold seep triggered by a hot ridge subduction.
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- Scientific Reports, 2021, v. 11, n. 1, p. 1, doi. 10.1038/s41598-021-00414-3
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- Article
Megathrust reflectivity reveals the updip limit of the 2014 Iquique earthquake rupture.
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- Nature Communications, 2022, v. 13, n. 1, p. 1, doi. 10.1038/s41467-022-31448-4
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Seismic structure of the north-central Chilean convergent margin: Subduction erosion of a paleomagmatic arc.
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- Geophysical Research Letters, 2014, v. 41, n. 5, p. 1523, doi. 10.1002/2013GL058729
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- Article
Reloca Slide: an ~24 km<sup>3</sup> submarine mass-wasting event in response to over-steepening and failure of the central Chilean continental slope.
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- Terra Nova, 2016, v. 28, n. 4, p. 257, doi. 10.1111/ter.12216
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Relationship Between Subduction Erosion and the Up‐Dip Limit of the 2014 Mw 8.1 Iquique Earthquake.
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- Geophysical Research Letters, 2021, v. 48, n. 9, p. 1, doi. 10.1029/2020GL092207
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2‐D V<sub>p</sub> and V<sub>s</sub> Models of the Indian Oceanic Crust Adjacent to the NinetyEast Ridge.
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- Journal of Geophysical Research. Solid Earth, 2023, v. 128, n. 3, p. 1, doi. 10.1029/2022JB025701
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Deep seismic structure of the Tonga subduction zone: Implications for mantle hydration, tectonic erosion, and arc magmatism.
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- Journal of Geophysical Research. Solid Earth, 2011, v. 116, n. B10, p. n/a, doi. 10.1029/2011JB008434
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Upper lithospheric structure of the subduction zone offshore of southern Arauco peninsula, Chile, at ∼38°S.
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- Journal of Geophysical Research. Solid Earth, 2008, v. 113, n. B7, p. n/a, doi. 10.1029/2007JB005569
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Morphology and geology of the continental shelf and upper slope of southern Central Chile (33°S-43°S).
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- International Journal of Earth Sciences, 2014, v. 103, n. 7, p. 1765, doi. 10.1007/s00531-012-0795-y
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The structure of the 2014 Mw 8.1 Iquique earthquake revealed by offshore observations.
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- Geophysical Research Abstracts, 2019, v. 21, p. 1
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Gravitational deformation and inherited structural control on slope morphology in the subduction zone of north-central Chile ( ca. 29-33°S).
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- Basin Research, 2017, v. 29, n. 6, p. 798, doi. 10.1111/bre.12205
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Alteration of the subducting oceanic lithosphere at the southern central Chile trench-outer rise.
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- Geochemistry, Geophysics, Geosystems: G3, 2007, v. 8, n. 7, p. n/a, doi. 10.1029/2007GC001632
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Active Tectonics of the North Chilean Marine Forearc and Adjacent Oceanic Nazca Plate.
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- Tectonics, 2018, v. 37, n. 11, p. 4194, doi. 10.1029/2018TC005087
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Tectonic control on sediment accretion and subduction off south central Chile: Implications for coseismic rupture processes of the 1960 and 2010 megathrust earthquakes.
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- Tectonics, 2010, v. 29, n. 6, p. n/a, doi. 10.1029/2010TC002734
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- Article