Littérature scientifique sur le sujet « Outer forearc high »
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Articles de revues sur le sujet "Outer forearc high":
Genge, Marie Catherine, César Witt, Frank Chanier, Jean-Yves Reynaud et Ysabel Calderon. « Outer forearc high control in an erosional subduction regime : The case of the central Peruvian forearc (6–10°S) ». Tectonophysics 789 (août 2020) : 228546. http://dx.doi.org/10.1016/j.tecto.2020.228546.
Tréhu, Anne M., Bridget Hass, Alexander de Moor, Andrei Maksymowicz, Eduardo Contreras-Reyes, Emilio Vera et Michael D. Tryon. « Geologic controls on up-dip and along-strike propagation of slip during subduction zone earthquakes from a high-resolution seismic reflection survey across the northern limit of slip during the 2010 Mw 8.8 Maule earthquake, offshore Chile ». Geosphere 15, no 6 (7 novembre 2019) : 1751–73. http://dx.doi.org/10.1130/ges02099.1.
Zhu, Gaohua, Hongfeng Yang, Jian Lin, Zhiyuan Zhou, Min Xu, Jinlong Sun et Kuiyuan Wan. « Along-strike variation in slab geometry at the southern Mariana subduction zone revealed by seismicity through ocean bottom seismic experiments ». Geophysical Journal International 218, no 3 (10 juin 2019) : 2122–35. http://dx.doi.org/10.1093/gji/ggz272.
BouDagher-Fadel, Marcelle K., G. David Price, Xiumian Hu et Juan Li. « Late Cretaceous to early Paleogene foraminiferal biozones in the Tibetan Himalayas, and a pan-Tethyan foraminiferal correlation scheme ». Stratigraphy 12, no 1 (2015) : 67–91. http://dx.doi.org/10.29041/strat.12.1.05.
Ayadh, Meriem, Amaury Guillermin, Marie-Angèle Abellan, Sara Figueiredo, Mélanie Pedrazzani, Emmanuel Cohen, Armelle Bigouret et Hassan Zahouani. « Investigation of the link between the human skin relief and the dermal fibers network by coupling topographic analysis and LC-OCT imaging before and during folding tests ». 4open 6 (2023) : 6. http://dx.doi.org/10.1051/fopen/2023005.
Vilas Boas, Juliana, Teresa Pereira, César Magalhães et Celeste Brito. « Dermatite de Contato Alérgica Ocupacional a múltiplos agentes num Canalizador ». Revista Portuguesa de Saúde Ocupacional 16 (31 décembre 2023) : esub0403. http://dx.doi.org/10.31252/rpso.08.07.2023.
Vako, Ilia. « Modern video recording systems of motor techniques : practical aspect ». Pedagogy and Psychology of Sport 5, no 1 (24 juin 2019) : 121–30. http://dx.doi.org/10.12775/pps.2019.05.01.008.
Johnston, Scott M., et Andrew R. C. Kylander-Clark. « Outer forearc uplift and exhumation during high-flux magmatism : Evidence from detrital zircon geochemistry of the Nacimiento forearc basin, California, USA ». Geology, 5 avril 2021. http://dx.doi.org/10.1130/g48627.1.
Watt, Janet T., et Daniel S. Brothers. « Systematic characterization of morphotectonic variability along the Cascadia convergent margin : Implications for shallow megathrust behavior and tsunami hazards ». Geosphere, 20 novembre 2020. http://dx.doi.org/10.1130/ges02178.1.
Wang, Zewei, Dapeng Zhao et Xiaofei Chen. « Fine Structure of the Subducting Slab and the 2022 M 7.4 Fukushima–Oki Intraslab Earthquake ». Seismological Research Letters, 30 septembre 2022. http://dx.doi.org/10.1785/0220220234.
Thèses sur le sujet "Outer forearc high":
Aizprua, Carlos. « Structure et développement du bassin d'avant-arc du sud-ouest des Andes du Nord ». Electronic Thesis or Diss., Université de Lille (2018-2021), 2021. http://www.theses.fr/2021LILUR001.
The SW Ecuador‐NW Peru forearc region is the southernmost location, where the Caribbean large igneous province (CLIP) interacted with the South American margin since the Late Cretaceous. The accretion of the CLIP to the margin led to the entrapment of the North Andean crustal Sliver, conforming the underlying basement of the forearc region in Ecuador, whereas in NW Peru, forearc depocenters involve rocks of continental affinity. Many existing tectonic reconstructions have treated these two areas independently, largely based on their crustal affinities. In contrast, this study integrates previous studies into an analysis of unpublished seismic profiles, potential field data, outcrop stratigraphy, and recent studies dealing with the dynamics of allochthonous terrane accretion along continental margins. Our integrated approach shows that SW Ecuador was dominated by a Late Cretaceous deforming outer wedge, which may have constituted a remnant of a northeast or northwest dipping obliquely obducted oceanic block at the edge of the CLIP. This tectonic phase was governed by plate instability, affecting NW Peru and SW Ecuador, followed by reestablishment of the margin by early Eocene. The resulting margin configuration and the spatial distribution of the different tectonic elements seem to have played a key role in the further Cenozoic development of the forearc region. The model presented in this study proposes that the accretion of buoyant oceanic terranes may have had a profound impact on the early margin configuration of SW Ecuador and NW Peru and led to the development of localized but genetically related forearc depocenters
Chapitres de livres sur le sujet "Outer forearc high":
Unruh, Jeffrey. « Upper plate deformation during blueschist exhumation, ancestral western California forearc basin, from stratigraphic and structural relationships at Mount Diablo and in the Rio Vista Basin ». Dans Regional Geology of Mount Diablo, California : Its Tectonic Evolution on the North America Plate Boundary. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.1217(10).
Goldfinger, Eliot. « Miscellaneous Animals Skeleton ». Dans Animal Anatomy for Artists. Oxford University Press, 2004. http://dx.doi.org/10.1093/oso/9780195142143.003.0014.