Zobrazeno 1 - 10
of 19
pro vyhledávání: '"Alexis Moussine-Pouchkine"'
Publikováno v:
Terra Nova. 13:220-226
N–S to NW–SE-trending faults and reverse faults occur within the Palaeozoic Ahnet–Mouydir Basin of the Algerian Saharan Platform, located to the east of the West African Pan-African suture zone. Deformation and stratigraphic analysis show that
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::72273f6b559ee3d781631992889da604
https://doi.org/10.1046/j.1365-3121.2001.00344.x
https://doi.org/10.1046/j.1365-3121.2001.00344.x
Publikováno v:
Sedimentology. 48:767-789
In the uppermost Jurassic of the central part of the South-East Basin of France, an association of lime mudstone beds, calcarenite beds and coarse carbonate breccia bodies form an informal stratigraphical unit called the ‘Barre Tithonique’. In th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5593f5bbfac75dcc45ab558a165d4bb7
https://doi.org/10.1046/j.1365-3091.2001.00395.x
https://doi.org/10.1046/j.1365-3091.2001.00395.x
Publikováno v:
Sedimentology. 48:231-254
Uppermost Jurassic limestones of the South-East Basin (France) are organized into four facies associations that were deposited in four distinct zones: (1) peritidal lagoonal limestones; (2) bioclastic and reefal limestones; (3) pelagic lime mudstones
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8be13d5e54b5d7cdc302ffa2cc8c2d85
https://doi.org/10.1046/j.1365-3091.2001.00358.x
https://doi.org/10.1046/j.1365-3091.2001.00358.x
Autor:
Fritz Neuweiler, Joachim Reitner, Claude Monty, Mark Feldmann, Stan Awramik, Pierre-André Bourque, Simonetta Cirilli, Pascale Gautret, Jean Marcoux, Jean Claude Plaziat, Christian Défarge, Jean Trichet, James L. Pinckney, Janine Bertrand-Sarfati, Alexis Moussine-Pouchkine, Pamela Reid, Martina Merz-Preiß, Sébastien Labiaux, Aymon Baud, Volker Thiel, Walter Michaelis, Ursula Galling, Hartmut Mäcker, Gernot Arp, Jenny Krutschinna, Robert Riding, Greogory E. Webb, John S. Jell, André Freiwald, Manmohan Mohanti, Srikanta Das, Matthias Bergbauer, Gabriela Schumann-Kindel, Werner Manz, Ulrich Szewzyk
Publikováno v:
Facies. 36:195-284
During the first step of the very rapid and large scale lowest Triassic transgression , we note in different areas (S Alps, Taurus,Turkey, S Armenia, E Elburz, Iran, Central Iran and Central Afghanistan) the growth of domal stromatolites, thrombolite
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ddec0389940ce733f789d0d8b7470a5c
https://doi.org/10.1007/bf02536885
https://doi.org/10.1007/bf02536885
Publikováno v:
Journal of African Earth Sciences. 24:425-443
During two mapping campaigns in Algeria, in the eastern part of the northern edge of the Taoudenni Basin, the imprints of tectonic events in the sediments of the Neoproterozoic to Early Cambrian cover was observed. These were obviously linked to tect
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9418c636dc2a376b06905aef7e3c62fa
https://doi.org/10.1016/s0899-5362(97)00073-0
https://doi.org/10.1016/s0899-5362(97)00073-0
Autor:
Gilles Ruffet, Bejan Asanidzé, Alexis Moussine-Pouchkine, Lolij Sholpo, Michel Prévot, Valera P. Shcherbakov, Afthandil Goguitchaichvili, Pierre Camps, Valja V. Shcherbakova
Publikováno v:
Physics of the Earth and Planetary Interiors. 96:41-59
A 250-m thick volcanic sequence of some 63 Pliocene lava flows from Georgia (Akhalkalaki plateau) which was previously thought to record the Gauss-Matuyama reversal was re-studied in detail. About 400 oriented cores were sampled along four sub-vertic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0ddbc4c48d89e514aa942ac7b3812e80
https://doi.org/10.1016/0031-9201(95)03110-3
https://doi.org/10.1016/0031-9201(95)03110-3
Publikováno v:
Geophysical Journal International. 119:166-186
SUMMARY We have carried out a palaeomagnetic investigation of the upper middle Devonian marly limestone of the Hazzel Matti Formation outcropping at Meredoua in the northern Ahaggar in the Sahara Desert. the Givetian age of the formation is well cons
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ec9388a6ecfc386b4a211ff77d39731b
https://doi.org/10.1111/j.1365-246x.1994.tb00920.x
https://doi.org/10.1111/j.1365-246x.1994.tb00920.x
Publikováno v:
SEPM Journal of Sedimentary Research. 67
At the end of the Early Cambrian glacial event occurring on the West African craton, the tillite surface was marked, especially in the northeastern part of the Taoudenni basin, by noticeable topographic relief. After deglaciation, the eustatic rise i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6bbd59cbc2be2f4c0f30fbe32e197588
https://doi.org/10.1306/d426868a-2b26-11d7-8648000102c1865d
https://doi.org/10.1306/d426868a-2b26-11d7-8648000102c1865d
Autor:
Roland Trompette, Yves Bellion, Alexis Moussine-Pouchkine, Janine Bertrand-Sarfati, Pascal Affaton
Publikováno v:
The West African Orogens and Circum-Atlantic Correlatives ISBN: 9783642841552
The West African craton, as defined by Kennedy (1964), represents a very large area stabilized after the Eburnean orogeny, 2150±150 Ma ago (Black and Fabre 1983, Bessoles 1983). These old rocks outcrop today in two separate shields: the Reguibat Shi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b5ffc02b3f971e6b2a23fcacbfd5542f
https://doi.org/10.1007/978-3-642-84153-8_4
https://doi.org/10.1007/978-3-642-84153-8_4
Publikováno v:
Geology. 23:133
Ediacara-type body fossils are reported here for the first time from the West African craton in Algeria. This assemblage comprises medusoids comparable to Medusinites sp. and Nimbia , a trace fossil, and a new genus of body fossil with uncertain affi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::435e515a8b1fa1a36ba699fb0d0d2481
https://doi.org/10.1130/0091-7613(1995)023<0133:feffiw>2.3.co
https://doi.org/10.1130/0091-7613(1995)023<0133:feffiw>2.3.co