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pro vyhledávání: '"HANCE L."'
Akademický článek
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Autor:
Menning, M., Alekseev, A.S., Chuvashov, B.I., Davydov, V.I., Devuyst, F.-X., Forke, H.C., Grunt, T.A., Hance, L., Heckel, P.H., Izokh, N.G., Jin, Y.-G., Jones, P.J., Kotlyar, G.V., Kozur, H.W., Nemyrovska, T.I., Schneider, J.W., Wang, X.-D., Weddige, K., Weyer, D., Work, D.M.
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 2006 240(1):318-372
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
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Publikováno v:
In Tectonophysics 1999 309(1):161-177
Autor:
STREEL M., BELKA Z., DREESEN R., DURKINA A.V., GROOS UFFENORDE H., HANCE L., HARTKOPF FRÖDER C., HAYDUKIEWICZ J., KORN D., PIECHA M., PERRI, MARIA CRISTINA, SPALLETTA, CLAUDIA
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::8fd6fe156c768b58bf1e528fad52589a
http://hdl.handle.net/11585/17802
http://hdl.handle.net/11585/17802
Autor:
Streel M., Belka Z., Dreesen R., Durkina A. V., Groos Uffenorde H., Hance L., Hartkopf Fröder C., Haydukiewicz J., Korn D., Piecha M., PERRI, MARIA CRISTINA, SPALLETTA, CLAUDIA
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4094::a8e7f3d4ba6511b75d741f459d804969
http://hdl.handle.net/11585/17905
http://hdl.handle.net/11585/17905
The Livian Substage is about 3-4 Ma long and was defined as corresponding to the Cf5 Foraminifer Zone by Conil et al., 1977 (= MFZ12 Zone of Devuyst & Hance, in Poty et al., in press). Its base is taken at the base of the "Banc d’or de Bachant"?, a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::3927f2dd2f66affde65516d495f620ab
http://www.vliz.be/imisdocs/publications/241991.pdf
http://www.vliz.be/imisdocs/publications/241991.pdf
The quality exposure of Viséan rocks in southern Belgium, the diversity of facies, the pioneer palaeontological works that started in the mid 19th century and the development of the foraminifer, conodont and rugose corals zonations in the last decad
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::bd40f776409dc0ea38a09a9c4e3d14ba
http://www.vliz.be/imisdocs/publications/242000.pdf
http://www.vliz.be/imisdocs/publications/242000.pdf
The Moliniacian is the basal division of the Viséan in Belgium (regional Substage). Its base is identified by the entry of the foraminifer Eoparastaffella simplex in the Salet road section and correlates with the base of the Viséan Stage. Its top i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::df768940ce185e17da75526101eedde5
http://www.vliz.be/imisdocs/publications/241995.pdf
http://www.vliz.be/imisdocs/publications/241995.pdf
The Warnantian Substage is about 8 to 12 Ma long and was defined as corresponding to the Cf6 Foraminifer Zone by Conil et al., 1977 (= MFZ13 to MFZ15 Zones of Devuyst & Hance (in Poty et al., in press). Its base is taken at the base of the Bonne Rive
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::d5f02ef0af9bcf3121f947e39d09b666
http://www.vliz.be/imisdocs/publications/242001.pdf
http://www.vliz.be/imisdocs/publications/242001.pdf