Zobrazeno 1 - 10
of 21
pro vyhledávání: '"Joseph, Canerot"'
Publikováno v:
Bulletin de la Société Géologique de France. 184:621-629
In their recently published paper, C. Clerc et al . [2012] describe the geological setting of the Etang de Lherz peridotite body and give a short review of the associated clastic deposits, proposing a detailed analysis of the breccias cropping out in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4b28aecea15dec2a06ab00cae165d19e
https://doi.org/10.2113/gssgfbull.184.6.621
https://doi.org/10.2113/gssgfbull.184.6.621
Publikováno v:
Eclogae Geologicae Helvetiae. 99:49-64
The Amelie-les-Bains (Eastern Pyrenees) breccias, recently considered to be Paleocene deep marine deposits, are reinterpreted here as Plio-Quaternary karstic brecciated accumulations. The palaeontological, sedimentological and paleogeographical data
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c2b6fa7ced8e1a2bf59a6639136d439e
https://doi.org/10.1007/s00015-006-1175-z
https://doi.org/10.1007/s00015-006-1175-z
Publikováno v:
AAPG Bulletin. 89:211-229
The Mesozoic history of the Pyrenean region was dominated by the opening of the North Atlantic Ocean and the left-lateral movement of Iberia relative to Europe. Most deformation was tensional or transtensional, but this style was interrupted by sever
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ce717fd9a9ea1f8eddba60c45d1802a9
https://doi.org/10.1306/09170404007
https://doi.org/10.1306/09170404007
Publikováno v:
Journal of African Earth Sciences. 39:393-400
A comparative study of the Middle Liassic series in the south western part of the Middle Atlas system leads to the definition of three new formations called Fellat 1, 2 and 3. They mainly involve gravity-flow deposits related to the breakup of the re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::beaf5058e34176b5945c68a62ab9ea43
https://doi.org/10.1016/j.jafrearsci.2004.07.028
https://doi.org/10.1016/j.jafrearsci.2004.07.028
Publikováno v:
Journal of African Earth Sciences. 39:337-346
The Moroccan Central High Atlasic mud-mounds correspond to carbonate sponge–algal buildups developed in open marine conditions towards the Lower–Upper Sinemurian boundary. The structures gradually increase in size through time, from the small-siz
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::07da2f5173e4bcc92d80d7f9e43c7b7b
https://doi.org/10.1016/j.jafrearsci.2004.07.063
https://doi.org/10.1016/j.jafrearsci.2004.07.063
Publikováno v:
Journal of African Earth Sciences
The cartographic, sedimentologic and stratigraphic studies carried out on the Mesozoic deposits in the border zone between the Middle and the High Moroccan Atlas (regions of Naour and Aghbala) led us to specify the lithology of formations, the signif
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::368c5506148927544c88e6821a772a77
https://doi.org/10.1016/s0899-5362(02)00027-1
https://doi.org/10.1016/s0899-5362(02)00027-1
Autor:
Joseph Canerot
Publikováno v:
BSGF-Earth Sciences Bulletin, Vol 188, Iss 6, p 35 (2017)
Contrary to recent conceptual models, we evidence that the Mauléon Basin does not only result from the Pyrenean tectonic inversion of an aborted Albian rift involving a N-S extreme crust thinning, with related detachment and mantle exhumation. It ac
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::beebb2c78a1dcc009dd18ab0b79fed16
https://doi.org/10.1051/bsgf/2017198
https://doi.org/10.1051/bsgf/2017198
Publikováno v:
Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science. 328:451-456
In the Western Pyrenees, the recent discovery of intra-Jurassic bauxites is not documented. In the present work, the authors show that the North-Pyrenean alterites are involved in two different Lower Cretaceous regression/transgression cycles related
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a5275615da053e6e55db5d2efca5f4cd
https://doi.org/10.1016/s1251-8050(99)80145-1
https://doi.org/10.1016/s1251-8050(99)80145-1
Publikováno v:
Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science. 326:723-728
New data from the Sierra Madre Oriental, in the Metztitlan, Xilitla and Sierra de El Abra areas, indicate a gradual, homoclinal ramp-type evolution from the Lower Cretaceous thin bedded outer-shelf Tamaulipas limestones to the Mid-Cretaceous massive
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1393e3bcaaf0277a4ee7a8c817a0de84
https://doi.org/10.1016/s1251-8050(98)80184-5
https://doi.org/10.1016/s1251-8050(98)80184-5
Publikováno v:
Geodinamica Acta
Geodinamica Acta, Taylor & Francis, 2007, 20 (6), pp.403-413. ⟨10.3166/ga.20.403-413⟩
Geodinamica Acta, Taylor & Francis, 2007, 20 (6), pp.403-413. ⟨10.3166/ga.20.403-413⟩
International audience
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e69f98be19eefee3c192ef0cfa42dc55
https://hal.archives-ouvertes.fr/hal-00319734
https://hal.archives-ouvertes.fr/hal-00319734
