Stratigraphie Corrélations Between the Continental and Marine Tethyan and Peri-Tethyan Basins During the Late Carboniferous and the Early Permian
Stratigraphie corrélations between the continental and marine Tethyan and Peri-Tethyan basins during the Late Carboniferous and the Early Permian Alain IZART 0), Denis VASLET <2>, Céline BRIAND (1>, Jean BROUTIN <3>, Robert COQUEL «>, Vladimir DAVYDOV («>, Martin DONSIMONI <2>, Mohammed El WARTITI <6>, Talgat ENSEPBAEV <7>, Mark GELUK <8>, Nathalya GOREVA <9), Naci GÔRÙR <1°>, Nayyer IQBAL <11>, Geroi JOLTAEV <7>, Olga KOSSOVAYA <12>, Karl KRAINER <13>, Jean-Pierre LAVEINE <«>, Maria MAKHLINA <14>, Alexander MASLO <15>, Tamara NEMIROVSKAYA <15>, Mahmoud KORA (16>, Raissa KOZITSKAYA (15>, Dominique MASSA <17>, Daniel MERCIER <18>, Olivier MONOD <19>, Stanislav OPLUSTIL <20>, Jôrg SCHNEIDER <21), Hans SCHÔNLAUB <22), Alexander STSCHEGOLEV <15>, Peter SÙSS <23\ Daniel VACHARD <4>, Gian Battista VAI <24>, Anna VOZAROVA <25>, Tuvia WEISSBROD <26>, Albin ZDANOWSKI <27> (see appendix 2 for addresses) Izart A. et al. 1998. — Stratigraphie corrélations between the continental and marine Tethyan and Peri-Tethyan basins during the Late Carboniferous and the Early Permian, in Crasquin-Soleau S., Izart A., Vaslet D. & De Wever P. (eds), Peri-Tethys: stratigraphie cor- relations 2, Geodiversitas 20 (4) : 521-595. ABSTRACT The compilation of detailed stratigraphie, sedimentologic and paléontologie data tesulted in sttatigtaphic corrélations of matine and continental areas outeropping today in the Tethyan and Peti-Tethyan domains: (1) the base of the Moscovian would correspond to the base of the Westphalian C in the Peri-Tethyan domain and to the base of the Westphalian B in the Tethyan domain; (2) the Kasimovian, the Gzhelian and the Otenbutgian would cor respond in the northern Peri-Tethyan domain and Tethyan domain (Catnic Alps) tespectively to the eatly Stephanian, the late Stephanian and the KEYWORDS Autunian p.p., in the southern Peri-Tethyan domain to an undifferentiated Peri-Tethys, biostratigrapny, time interval.
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