Zobrazeno 1 - 10
of 56
pro vyhledávání: '"Lorenzo Colli"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 23, Iss 11, Pp n/a-n/a (2022)
Abstract Pacific‐Panthalassa plate tectonics are the most challenging on Earth to reconstruct during the Mesozoic and Cenozoic eras due to extensive subduction, which has resulted in large (>9,000 km length) unconstrained gaps between the Pacific a
Externí odkaz:
https://doaj.org/article/784d8115097c4252a255c82818e5f7c9
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
The tectonics of East Asia are notoriously complex. Consisting of an intricate patchwork of microplates and accreted terranes, even the Cenozoic tectonic history of the region remains controversial, and many differing reconstructions have been propos
Externí odkaz:
https://doaj.org/article/840c09bc6e514ba2a53903247c0733ff
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-9 (2021)
Here, the authors follow a new approach using analytic solutions for Poiseuille-Couette channel flow to compute asthenospheric viscosities under the Caribbean. Active asthenospheric flow observed under the Caribbean contradicts the traditional view t
Externí odkaz:
https://doaj.org/article/65d116ca11cb4c1cabc8f71a64d9be70
Seismic velocity anomalies observed in the mantle can have several origins, the main contributions being anomalies of temperature and composition. The difference between P- and S-wave models has been used to separate thermal and compositional contrib
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f715839596a36ad4ebce2812579c3cd3
https://doi.org/10.5194/egusphere-egu23-10123
https://doi.org/10.5194/egusphere-egu23-10123
It is generally accepted that East Asian mantle dynamics has been dominated by subduction and downwelling since Mesozoic times (e.g. Müller et al. (2016)). However, seemingly in contrast to this history, a variety of observations indicate a presence
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9286bb4c9707cb5b555bed901d1fd1ee
https://doi.org/10.5194/egusphere-egu23-3213
https://doi.org/10.5194/egusphere-egu23-3213
The plate tectonic history of the Pacific Ocean and its predecessor ocean, Panthalassa, are challenging regions on Earth to reconstruct during the Mesozoic-Cenozoic eras. More than 95% of Pacific-Panthalassa crust has been subducted into the Earth’
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a850c582917ce47f406c942dbb0c040a
https://doi.org/10.5194/egusphere-egu23-10007
https://doi.org/10.5194/egusphere-egu23-10007
One of the greatest challenges of modeling the plate tectonic history of Earth during the Mesozoic and Cenozoic eras lies in reconstructing the Pacific Ocean and its predecessor ocean, Panthalassa. A major reason for the plate tectonic uncertainty in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ce73f481b3e85650ccc2b5f7a0ad6ddb
https://doi.org/10.5194/egusphere-egu22-10560
https://doi.org/10.5194/egusphere-egu22-10560
The tectonics of East and Southeast Asia are notoriously complex. Consisting of an intricate patchwork of microplates and accreted terrains, even the recent (i.e Cenozoic) tectonic history of the region remains controversial; and many differing recon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d6bc6c0aba742e2e93a0ac743f7b7c85
https://doi.org/10.5194/egusphere-egu22-1896
https://doi.org/10.5194/egusphere-egu22-1896
Autor:
T. Greenfield, D. Rhodri Davies, Simone Pilia, Nicholas Rawlinson, Cian R. Wilson, Felix Tongkul, Lorenzo Colli, Stephan C. Kramer, David G. Cornwell, Robert Hall, A. Gilligan, Conor Bacon
Subduction is a key driver of plate tectonics on Earth1. A range of observations indicate that the termination of subduction leads to diverse and unexplained tectonic and geological activity, including anomalous magmatism, exhumation and topographic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f54453147eba6e6f6b2fe7905bf3e142
https://doi.org/10.21203/rs.3.rs-861968/v1
https://doi.org/10.21203/rs.3.rs-861968/v1