Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Arnaud Broussolle"'
Autor:
Arnaud Broussolle
Publikováno v:
Scientific Reports, Vol 12, Iss 1, Pp 1-8 (2022)
Abstract The supercontinent cycle has been the focus of researchers for many years, but the parameters of its cyclicity remain a central debate; thus, prediction of the occurrence of the next supercontinent remains elusive. In this research, a mathem
Externí odkaz:
https://doaj.org/article/ebe1b02ecdd648f1a751b67330cc0f30
Autor:
Arnaud Broussolle
Publikováno v:
Scientific reports. 12(1)
The supercontinent cycle has been the focus of researchers for many years, but the parameters of its cyclicity remain a central debate; thus, prediction of the occurrence of the next supercontinent remains elusive. In this research, a mathematical po
Autor:
Yang Yu, Jin-Hui Yang, Arnaud Broussolle, Alfred Kröner, Xiaoping Long, Guochun Zhao, Pengfei Li, Min Sun
Publikováno v:
Gondwana Research. 47:131-141
The nature of the lower crust and tectonic setting of the Chinese Altai in the early to middle Paleozoic are still hotly debated. Decoupling between zircon Hf and whole-rock Nd isotopic systems for granites results in different interpretations for th
Autor:
Pavla Štípská, Arnaud Broussolle, Yingde Jiang, Karel Schulmann, Min Sun, Yang Yu, Alexandra Guy, Wenjiao Xiao, Carmen Aguilar
Publikováno v:
Gondwana Research
Gondwana Research, Elsevier, 2019, 66, pp.183-206. ⟨10.1016/j.gr.2018.11.003⟩
Dipòsit Digital de la UB
Universidad de Barcelona
Gondwana Research, Elsevier, 2019, 66, pp.183-206. ⟨10.1016/j.gr.2018.11.003⟩
Dipòsit Digital de la UB
Universidad de Barcelona
The general structure of the Chinese Altai has been traditionally regarded as being formed by five tectono-stratigraphic ‘terranes’ bounded by large-scale faults. However, numerous detrital zircon studies of the Paleozoic volcano-sedimentary sequ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::88c9548e70a2dfbbf59ee0a699f6169f
https://hal.archives-ouvertes.fr/hal-02469117
https://hal.archives-ouvertes.fr/hal-02469117
Publikováno v:
Journal of Asian Earth Sciences. 203:104538
A debate exists on whether the deep crust of the Altai Orogenic Belt contains ancient crustal components. To further address this issue, geochemical analyses and zircon hafnium isotopic measurements were conducted on five Devonian magmatic rocks from
Autor:
Yingde Jiang, Arnaud Broussolle, Wenjiao Xiao, Karel Schulmann, Sheng Wang, Yang Yu, Pavla Štípská, Jitka Míková, Carmen Aguilar, Min Sun
Publikováno v:
Lithos
Lithos, Elsevier, 2018, 314-315, pp.400-424. ⟨10.1016/j.lithos.2018.06.005⟩
Dipòsit Digital de la UB
Universidad de Barcelona
Lithos, Elsevier, 2018, 314-315, pp.400-424. ⟨10.1016/j.lithos.2018.06.005⟩
Dipòsit Digital de la UB
Universidad de Barcelona
Structural analysis and U–Pb geochronological study on zircons from the southern Chinese Altai (the Kalasu area, SE of the Altai city) show that the Cambro-Ordovician accretionary wedge (ca. 520–492 Ma) underwent four major geological events: 1)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::213a6439ad2dc8bc603e69c1a3388d21
https://hal.archives-ouvertes.fr/hal-01896696
https://hal.archives-ouvertes.fr/hal-01896696
Autor:
Bradley R. Hacker, Karel Schulmann, Pavlína Hasalová, Jérémie Lehmann, Ondrej Lexa, Martin Racek, David Buriánek, Andrew R.C. Kylander-Clark, Pavel Hanžl, Kristýna Hrdličková, Arnaud Broussolle, Pavla Štípská, Robert M. Holder
Publikováno v:
Journal of Metamorphic Geology
Journal of Metamorphic Geology, Wiley-Blackwell, 2015, 33 (359-383), ⟨10.1111/jmg.12124⟩
Journal of Metamorphic Geology, Wiley-Blackwell, 2015, 33 (359-383), ⟨10.1111/jmg.12124⟩
The Chandman massif, a typical structure of the Mongolian Altai, consists of a migmatite–magmatite core rimmed by a lower grade metamorphic envelope of andalusite and cordierite-bearing schists. The oldest structure in the migmatite–magmatite cor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::94237269dc792a50b98e7621e1910f54
https://hal.archives-ouvertes.fr/hal-01213914
https://hal.archives-ouvertes.fr/hal-01213914