Peer-reviewed articles 17,970 +



Title: DISTRIBUTION OF CRETACIC / MIOCENE PETROFACIES AT THE CONTACT OF THE CARPATHIAN OROGENE AND MOLDAVIAN PLATFORM. MORPHOMETRIC PARTICULARITIES OF THE MOUNTAIN-PLATEAU RELIEF TRANSITION, BETWEEN SUCEAVA AND MOLDOVA VALLEY (OBCINA MARE/SUCEAVA PLATEAU, ROMANI

DISTRIBUTION OF CRETACIC / MIOCENE PETROFACIES AT THE CONTACT OF THE CARPATHIAN OROGENE AND MOLDAVIAN PLATFORM. MORPHOMETRIC PARTICULARITIES OF THE MOUNTAIN-PLATEAU RELIEF TRANSITION, BETWEEN SUCEAVA AND MOLDOVA VALLEY (OBCINA MARE/SUCEAVA PLATEAU, ROMANI
J. D. Toader;U. Adrian;C. Ciprian;J. Valentin
1314-2704
English
19
1.1
The geotectonic events in Late Cretaceous - Early Paleogene interval, caused
essential changes in the architecture of the Tethysian paleogenic sedimentation basins
and their rela relationship with the continental source areas. Laramic tectogenetic paroxysm
(Maastrich tian/Danian) due to the subductin of the East European craton under the
TiszaTisza-Dacia block, plays a double role in the structuralization of the East Carpathian
units. In an internal position, the External Dacides are built (The Black Flysch, Baraolt,
CeahlCeahlau and Bobu nappes, senso Sandulescu, 1984), and in the external part the
Paleogene Foreland basin depozones (equivalent to the "Foreland basin", senso Grasu et
al. , The basin worked up to the Lower Miocene, when the styric and moldavic
tectogenesis occurred and the Moldavian units were born (from the inner part to the
outside are: Marginal Folds Nappe, Macla Nappe, Audia Nappe, Tarcau Nappe, Vrancea
Nappe and Subcarp Subcarpathian Nappe, senso Sandulescu [ 1], 1984). The Moldavian
tectogenesis (intra Volhini an) concludes the Carpathian structogenesis and edification of
the major morphostructural lines of the Carpathian contact with the eastern foreland.
Between the Suceava and Mod ova valleys, the transition from the mountainous relief
(Obcina Mare) to the pla teau is made through the piedmont hills formed on the sub sub-Carpathian molasse or the Volhinian platform couverture deposits, accumulated on the
wedgewedge-top of the Carpathian orogenic prism.
conference
19th International Multidisciplinary Scientific GeoConference SGEM 2019
19th International Multidisciplinary Scientific GeoConference SGEM 2019, 30 June - 6 July, 2019
Proceedings Paper
STEF92 Technology
International Multidisciplinary Scientific GeoConference-SGEM
Bulgarian Acad Sci; Acad Sci Czech Republ; Latvian Acad Sci; Polish Acad Sci; Russian Acad Sci; Serbian Acad Sci & Arts; Slovak Acad Sci; Natl Acad Sci Ukraine; Natl Acad Sci Armenia; Sci Council Japan; World Acad Sci; European Acad Sci, Arts & Letters; Ac
147-162
30 June - 6 July, 2019
website
cdrom
4791
Moldavides; petrofacies; post post-Moldavian morphogenesis; Obci na
Mare/Moldova Plateau contact.