Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Luc Hance"'
Autor:
PAUL L. BRENCKLE, LUC HANCE
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 111, Iss 2 (2005)
Hastarian formations in southern Belgium contain previously undescribed or unfigured foraminiferal taxa that provide a link to better known early Tournaisian faunas from eastern Europe. Characteristic specimens are illustrated, and selected elements
Externí odkaz:
https://doaj.org/article/b67359009c9243b4b1ecd45df5a02980
Publikováno v:
Palaeobiodiversity and Palaeoenvironments. 101:313-356
The Devonian–Carboniferous boundary is associated with a major extinction event of the Phanerozoic. It was also a time marked by a rapid but short-lasting change in deposition called Hangenberg Event. In the Namur–Dinant Basin the uppermost Devon
Autor:
Jean-Marc Marion, Luc Hance, Julien Denayer, Valentin Fischer, Emmanuel Chevalier, Markus Aretz, Bernard Mottequin, Laurent Barchy
Publikováno v:
Geologica Belgica. 19:3-6
‘Generalist’ is a qualifying word that best describes Edouard – ‘Eddy’ – Poty in term of knowledge. He is not just a well-known palaeontologist. Passionate in all branches of geology, he developed an exceptional background and became one
Publikováno v:
Geological Magazine. 151:229-243
The Tournaisian and Viséan were formerly considered as series and in Belgium were divided into two (Hastarian and Ivorian) and three stages (Moliniacian, Livian and Warnantian), which are now considered as substages. The Belgian substages are based
Publikováno v:
Geological Journal. 47:450-461
For the first time Waulsortian-like carbonate mud banks are described from lower Mississippian strata of South China. The carbonate mud banks occur in the upper member of the Long'an Formation (late Tournaisian in age) at Longdianshan Hill (near Liuz
Autor:
Hongfei Hou, Xianghe Wu, Francois-Xavier Devuyst, Michel Coen, Luc Hance, George D. Sevastopulo, Shugang Tian
Publikováno v:
Episodes. 26:105-115
The first appearance of Eoparastaffella simplex in the lineage Eoparastaffella ovalis - Eoparastaffella simplex (foraminifers) has been officially approved by the Voting Members of the SCCS in early 2002 as the new biostratigraphic criterion to defin
Publikováno v:
Geologica Belgica. 4:69-94
Six paleogeographic sedimentation areas (s. a.) are recognized in the Namur-Dinant Basin: (1) the Hainaut s. a., (2) the Namur s. a., (3) the Condroz s. a., (4) the Dinant s. a., (5) the Visé-Maastricht s. a., and (6) the southern Avesnois s. a. (on
Publikováno v:
Geologica Belgica. 3:285-307
Strata of late Devonian and Tournaisian age in Belgium and Southern China were studied sedimentologically. This detailed study integrated into a biostratigraphical framework, based on foraminiferal zonation, allowed the construction of a sequence str
Publikováno v:
Bulletin de la Société Géologique de France. 172:411-426
The relative influences of local tectonics and global eustasy in the architecture of the sedimentary units of the Namur-Dinant Basin (southern Belgium) are determined. Nine third-order sequences are recognised. During the Lower Tournaisian (Hastarian
Publikováno v:
Tectonophysics. 309:161-177
The ramp-flat thrust model and other classical models based on Rocky ountains or Appalachians structures allow a better understanding of ault and fold interaction in a sequence dominated by competent rocks, n which, in most cases, thrusts propagate f