Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Nicholas Schliffke"'
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-7 (2022)
Back-arc spreading centre jumps have been suggested to be controlled by a number of different drivers. Here, the authors, using 3D numerical models, show that transform faults can trigger back-arc spreading centre jumps, without the need of any ad ho
Externí odkaz:
https://doaj.org/article/916d41c892fc443883c96a7266dfeb44
Autor:
Solenn Hertgen, Philippe Yamato, Benjamin Guillaume, Valentina Magni, Nicholas Schliffke, Jeroen vanHunen
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 21, Iss 2, Pp n/a-n/a (2020)
Abstract The important role played by the upper plate in convergence zones dynamics has long been underestimated but is now more and more emphasized. However, the influence of its thickness and/or strength on orogenic systems evolution remains largel
Externí odkaz:
https://doaj.org/article/c6689bbb499e45d3a836c3c003ee0226
Autor:
Valentina Magni, Nicholas Schliffke, Jeroen van Hunen, Frédéric Gueydan, Mark Allen, John Naliboff, Manel Prada, Carmen Gaina
The structure of oceanic back-arc basins reflects the dynamics of the subduction zone they are associated with. Often, the basement of these basins is not only composed of oceanic crust, but also of exhumed mantle, fragments of continental crust, int
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a202d44656e225376fe49e59c3928b78
https://doi.org/10.5194/egusphere-egu22-4810
https://doi.org/10.5194/egusphere-egu22-4810
Autor:
Nicholas Schliffke
Detailed figures of the model evolution, as well as a short description of the methodology and parameters used.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::00dabe11fda95e7ca7cdb74312f8a4e8
https://doi.org/10.1130/geol.s.15062262
https://doi.org/10.1130/geol.s.15062262
Publikováno v:
Geochemistry, geophysics, geosystems, 2019, Vol.20(11), pp.4693-4709 [Peer Reviewed Journal]
Geochemistry, Geophysics, Geosystems : G(3)
Geochemistry, Geophysics, Geosystems : G(3)
During continental collision, considerable amounts of buoyant continental crust subduct to depth and subsequently exhume. Whether various exhumation paths contribute to contrasting styles of magmatism across modern collision zones is unclear. Here we
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2901707c047d371e4c7a04ff0c13067c
https://doi.org/10.1029/2019gc008590
https://doi.org/10.1029/2019gc008590
Jumps in the location of back-arc spreading centres are a common feature of back-arc basins, but the controlling factors are not understood. In several narrow subduction zones with a long subduction history, such as the Scotia arc or Tyrhennian Sea,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0b2575c1637b9bd7ce0a42a23bc8efd1
https://doi.org/10.5194/egusphere-egu2020-16952
https://doi.org/10.5194/egusphere-egu2020-16952