Anticlockwise metamorphic paths at ca. 890–790 Ma from the NE Baidrag block, Mongolia, indicate back-arc compression at the Rodinia periphery

Autor: Pavla Štípská, Vít Peřestý, Igor Soejono, Karel Schulmann, R.C. Andrew Kylander–Clark, Carmen Aguilar, Stephen Collett, Martin Racek, Jitka Míková, Otgonbaatar Dorjsuren, Nikol Novotná

Publikováno v: Geoscience Frontiers. 14:101520

The processes leading to the assembly of the Rodinia supercontinent through Grenvillian collisional orogeny are relatively well known. In contrast, accretionary orogenic processes occurring at the supercontinent periphery following Rodinia assembly a

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::139bd348b03a6979bdf8c04b49ccb08e
https://doi.org/10.1016/j.gsf.2022.101520

The enriched Variscan lithosphere of NE Iberia: data from postcollisional Permian calc-alkaline lamprophyre dykes of Les Guilleries

Autor: Esteban Mellado, Mercè Corbella, Didac Navarro, Andrew Kylander

Publikováno v: Geologica Acta; Vol. 19 (2021); 1-23
RCUB. Revistas Científicas de la Universidad de Barcelona
Agencia Estatal de Meteorología (AEMET)
Dipòsit Digital de Documents de la UAB
Universitat Autònoma de Barcelona
Dipòsit Digital de la UB
Universidad de Barcelona

Post-collisional mafic dykes crosscut the Paleozoic metamorphic basement and late-Variscan plutons in Les Guilleries massif (Catalan Coastal Ranges, NE Iberia). The predominance of mafic phenocrysts, porphyritic texture, abundant amphibole, high MgO

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4d48ddf2a02e9eb7df7a7545c02150d7
http://revistes.ub.edu/index.php/GEOACTA/article/view/34109

Growth of Collisional Orogens From Small and Cold to Large and Hot—Inferences From Geodynamic Models

Autor: Peter van der Beek, M. E. Curry, Sebastian G. Wolf, Ritske S. Huismans, Josep Anton Muñoz

Publikováno v: e2020JB021168
Journal of Geophysical Research (JGR): Solid Earth
Dipòsit Digital de la UB
Universidad de Barcelona

It is well documented that the interplay between crustal thickening and surface processes determines growth of continent-continent collision orogens from small and cold to large and hot. Additionally, studies have demonstrated that the structural sty

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3148daf3af783890c6135f80f90dfd06
https://doi.org/10.1029/2020jb021168

Contrasting P-T-t-d paths of the polycyclic Palaeozoic tectono-metamorphic event in the Southern Chinese Altai: an example from Kalasu area

Autor: Broussolle, Arnaoud, Aguilar Gil, Carmen María, Sun, Min, Stípská, Pavla, Schulmann, Karel, Jiang, Yingde, Yu, Yang, Xiao, Wenjiao

Publikováno v: Dipòsit Digital de la UB
Universidad de Barcelona

To understand the polycyclic Palaeozoic tectono-metamorphic evolution of the Southern Chinese Altai, petrological and structural studies together with thermodynamic modelling and dating were carried out in the Cambro-Ordovician metapelitic sequence o

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::895242bf4b4fc29cfd5d6a1fbb198dc2
http://hdl.handle.net/2445/183337

Structural and geochronological evolution of an accretionary orogenic wedge during Altai orogeny: An example from the Kalasu area (Chinese Altai)

Autor: Broussolle, Arnaoud, Aguilar Gil, Carmen María, Sun, Min, Schulmann, Karel, Stípská, Pavla, Jiang, Yingde, Yu, Yang, Wang, Sheng, Míková, Jitka

Publikováno v: Dipòsit Digital de la UB
Universidad de Barcelona

A detailed geological and structural mapping was carried out in the Kalasu area located in the southern Chinese Altai, a small segment of the giant Altai accretionary orogenic wedge, in order to understand its polycyclic evolution. The Kalasu area is

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::fc097c2bb718527db536748ecd265f91
http://hdl.handle.net/2445/183336