Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Goran Andjić"'
Publikováno v:
Communications Earth & Environment, Vol 3, Iss 1, Pp 1-7 (2022)
The formation and tectonic evolution of mafic oceanic crust can be determined through dating of calcite amygdules using U-Pb geochronology as well as geochemistry and biostratigraphic observations, according to a study of the New England Orogen, Aust
Externí odkaz:
https://doaj.org/article/ed589b49b41741f8959305bbdf6eda24
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 23, Iss 3, Pp n/a-n/a (2022)
Abstract Tectonic interpretations of arc remnants in the Himalayan orogen remain uncertain, despite their important implications for the overall convergence history between India and Eurasia. Provenance results from deep‐water volcaniclastic rocks
Externí odkaz:
https://doaj.org/article/960cd666c9c44caf9a3d9988cd19061f
Publikováno v:
Geochemistry, Geophysics, Geosystems. 23
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::308394707dbbc9268054c203d757d9b6
https://doi.org/10.1029/2021gc010042
https://doi.org/10.1029/2021gc010042
Publikováno v:
Tectonics. 40
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::716cd0e3a640bde162e0fc31aa02f8e4
https://doi.org/10.1029/2021tc006920
https://doi.org/10.1029/2021tc006920
Autor:
Simon F. Mitchell, Peter Baumgartner, Michèle Caron, Esmeralda Caus, Javier Escuder-Viruete, Goran Andjić, Claudia Baumgartner-Mora
Publikováno v:
Tectonics. 38:4399-4425
The western margin of the Caribbean Plate is a typical example where oceanic and continental terranes have amalgamated by subduction, collision, and strike-slip processes. The boundaries between these blocks, as well as their tectonostratigraphic rec
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b5ebd746002382bd15f22f00a2cbb95c
https://doi.org/10.1029/2019tc005741
https://doi.org/10.1029/2019tc005741
Publikováno v:
GSA Bulletin. 131:1555-1580
The Cretaceous period was marked by the most voluminous episodes of oceanic plateau volcanism in the Phanerozoic Eon. Primarily affecting the Pacific, mantle plumes generated oceanic plateaus during three main phases (ca. 145–140 Ma, ca. 122–115
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::423e29589542f2019deef9fd2a3ccbea
https://doi.org/10.1130/b35037.1
https://doi.org/10.1130/b35037.1
Publikováno v:
Basin Research. 30:863-894
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7cae5c810bbc07eb254cec2368c7f1e8
https://doi.org/10.1111/bre.12284
https://doi.org/10.1111/bre.12284
Publikováno v:
The Depositional Record, vol. 4, pp. 90-132
The southern Central American active margin is a world-class site where past and present subduction processes have been extensively studied. Tectonic erosion/accretion and oblique/orthogonal subduction are thought to alternate in space and time along
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1d7d55455217bbebd88e04dc05ef2c52
https://doi.org/10.1002/dep2.40
https://doi.org/10.1002/dep2.40
Publikováno v:
Facies. 62
The Sandino Forearc Basin of western Nicaragua and northwestern Costa Rica (Central America) provides a Campanian to Pliocene sedimentary record. The study of the onshore part of the basin in northwestern Costa Rica reveals for the first time the occ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a752cdb0afb2717fc98a450eac2e3893
https://doi.org/10.1007/s10347-016-0463-y
https://doi.org/10.1007/s10347-016-0463-y