Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Antoine Demoux"'
Autor:
Ping Jian, Antoine Demoux, Dondov Tomurhuu, Matthias Barth, Yamirka Rojas-Agramonte, Thomas Zack, Alfred Kröner
Publikováno v:
Journal of Asian Earth Sciences. 42:1008-1017
Magmatic zircons from the basal part of an arc terrane in the accretionary complex NE of the Baydrag microcontinental block in central Mongolia were dated at 544 ± 7 Ma and reflect arc magmatism at the Ediacaran/Cambrian boundary. Detrital zircon ag
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7c2607007a577375603bc08e93214e4f
https://doi.org/10.1016/j.jseaes.2010.09.002
https://doi.org/10.1016/j.jseaes.2010.09.002
Autor:
Dunyi Liu, T. Donskaya, Xiaoping Xia, Antoine Demoux, Min Sun, Yamirka Rojas-Agramonte, W. Wang, Alfred Kröner
Publikováno v:
Gondwana Research. 19:751-763
The Central Asian Orogenic Belt contains many Precambrian crustal fragments whose origin is unknown, and previous speculations suggested these to be derived from either Siberia, Tarim or northern Gondwana. We present an age pattern for detrital and x
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0775cae107a8a1b044432434e3bb0c0f
https://doi.org/10.1016/j.gr.2010.10.004
https://doi.org/10.1016/j.gr.2010.10.004
Autor:
Antoine Demoux, Dondovyn Tomurhuu, Ping Jian, Michael T.D. Wingate, Alfred Kröner, Gombosuren Badarch
Publikováno v:
The Journal of Geology. 117:377-397
Central Mongolia represents a heterogeneous crustal domain of the Central Asian Orogenic Belt and is composed of contrasting lithotectonic units with distinct preorogenic histories. We report single-zircon evaporation and SHRIMP ages for high-grade r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2a829bf24e1227f3f3dda6c8f7c5a925
https://doi.org/10.1086/598947
https://doi.org/10.1086/598947
Publikováno v:
Journal of the Geological Society. 166:459-471
The Tseel terrane in the Gobi Desert of SW Mongolia consists of a composite crustal segment of imbricated sheets of high- and low-grade metamorphic rocks of predominantly middle Palaeozoic age. New sensitive high-resolution ion microprobe (SHRIMP) zi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::501d2ba8ce9f3e436bd64eb03522eb2a
https://doi.org/10.1144/0016-76492008-090
https://doi.org/10.1144/0016-76492008-090
Publikováno v:
International Journal of Earth Sciences. 98:1365-1380
Single zircon ages determined by ion microprobe (SHRIMP II) for granitoid gneisses from the southern slope of the Baga Bogd massif (Gobi-Altai, southern Mongolia) reveal several episodes of zircon growth, ranging from late Palaeoproterozoic to late C
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::79e8c53565121c6ffc971da7e1f95dec
https://doi.org/10.1007/s00531-008-0321-4
https://doi.org/10.1007/s00531-008-0321-4
Publikováno v:
International Journal of Earth Sciences
International Journal of Earth Sciences, 2010, 99 (2), pp.327-341. ⟨10.1007/s00531-008-0397-x⟩
International Journal of Earth Sciences, Springer Verlag, 2010, 99 (2), pp.327-341. ⟨10.1007/s00531-008-0397-x⟩
International Journal of Earth Sciences, 2010, 99 (2), pp.327-341. ⟨10.1007/s00531-008-0397-x⟩
International Journal of Earth Sciences, Springer Verlag, 2010, 99 (2), pp.327-341. ⟨10.1007/s00531-008-0397-x⟩
International audience; Detailed 40Ar/39Ar geochronology on single grains of muscovite was performed in the Variscan Tanneron Massif (SE France) to determine the precise timing of the post-collisional exhumation processes. Thirty-two plateau ages, ob
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c6cdb211bcdc5db67c596850f0342d73
https://hal.science/hal-00457220
https://hal.science/hal-00457220
Publikováno v:
Journal of the Geological Society of London
Journal of the Geological Society of London, Geological Society of London, 2008, 165 (2), pp.467-478. ⟨10.1144/0016-76492007-045⟩
Journal of the Geological Society of London, 2008, 165 (2), pp.467-478. ⟨10.1144/0016-76492007-045⟩
Journal of the Geological Society of London, Geological Society of London, 2008, 165 (2), pp.467-478. ⟨10.1144/0016-76492007-045⟩
Journal of the Geological Society of London, 2008, 165 (2), pp.467-478. ⟨10.1144/0016-76492007-045⟩
The Tanneron massif belongs to the southernmost segment of the Variscan belt in France and is composed of migmatitic orthogneisses and paragneisses cross-cut by a main tonalite–granite complex. Late Carboniferous detrital basins are bounded by nort
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::187aec5b599b59e1dc76cd9a2d8b3d29
https://hal.archives-ouvertes.fr/hal-00407866
https://hal.archives-ouvertes.fr/hal-00407866
Autor:
S. Gruschka, E.V. Khain, Michael T.D. Wingate, Antoine Demoux, Ernst Hegner, Alfred Kröner, Bor-ming Jahn, O. Tomurtogoo, Gombosuren Badarch, Brian F. Windley
Kroner, A., Windley, B.F., Badarch, G., Tomurtogoo, O., Hegner, E., Jahn, B.M., Gruschka, S., Khain, E.V., Demoux, A., and Wingate, M.T.D., 2007, Accretionary growth and crust formation in the Central Asian Orogenic Belt and comparison with the Arabi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e9df0e8a1593aef39b04f8e0273bb54d
https://doi.org/10.1130/2007.1200(11)
https://doi.org/10.1130/2007.1200(11)