Browsing ELibrary by Author "Saintot A."

Now showing items 1-7 of 7

CRUSTAL-SCALE POP-UP STRUCTURE IN CRATONIC LITHOSPHERE: DOBRE DEEP SEISMIC REFLECTION STUDY OF THE DONBAS FOLD BELT, UKRAINE

Maystrenko Y.; Stovba S.; Tolkunov A.; Stephenson R.; Saintot A.; Bayer U.; Menyoli E.; Gajewski D.; Huebscher C.; Rabbel W.; Starostenko V.; Thybo H. (2003)

The DOBRE project investigated the interplay of geologic and geodynamic processes that controlled the evolution of the Donbas fold belt, Ukraine, as an example of an inverted intracratonic rift basin. A deep seismic ...
EVOLUTION OF THE SOUTHERN MARGIN OF THE DONBAS (UKRAINE) FROM DEVONIAN TO EARLY CARBONIFEROUS TIMES

McCann T.; Saintot A.; Chalot-Prat F.; Kitchka A.; Fokin P.; Alekseev A. (2003)

A Devonian-Early Carboniferous succession comprising thick clastic and carbonate sediments with interbedded volcanics was examined along the southern margin of the Donbas fold belt. Ukraine. Following initial rifting and ...
PALEOSTRESS FIELD RECONSTRUCTION AND REVISED TECTONIC HISTORY OF THE DONBAS FOLD AND THRUST BELT (UKRAINE AND RUSSIA)

Saintot A.; Stephenson R.; Brem A.; Stovba S.; Privalov V. (2003)

In the WNW-ESE Donbas fold belt (DF), inversion of 3500 microtectonic data collected at 135 sites, in Proterozoic, Devonian, Carboniferous, and Cretaceous competent rocks allowed reconstruction of 123 local stress states. ...
STRUCTURES ASSOCIATED WITH INVERSION OF THE DONBAS FOLDBELT (UKRAINE AND RUSSIA)

Saintot A.; Stephenson R.; Stovba S.; Maystrenko Y. (2003)

The Donbas Foldbelt is part of the Prypiat–Dnieper–Donets intracratonic rift basin (Belarus–Ukraine–southern Russia) that developed in Late Devonian times and was reactivated in Early Carboniferous. To the southeast, the ...
TECTONIC PALEOSTRESS FIELDS AND STRUCTURAL EVOLUTION OF THE NW-CAUCASUS FOLD-AND-THRUST BELT FROM LATE CRETACEOUS TO QUATERNARY

Saintot A.; Angelier J. (2002)

The NW-Caucasus fold-and thrust belt essentially corresponds to the inverted western Flysch Zone of the Great Caucasus Mountains, a deep basin that developed from Late Jurassic to Eocene times between the Scythian Plate ...
THE 40AR/39AR DATING OF MAGMATIC ACTIVITY IN THE DONBAS FOLD BELT AND THE SCYTHIAN PLATFORM (EASTERN EUROPEAN CRATON)

Alexandre P.; Chalot-Prat F.; Saintot A.; Wijbrans J.; Stephenson R.; Wilson M.; Kitchka A.; Stovba S. (2004)

The Donbas Fold Belt is the compressionally deformed southeasternmost part of the intracratonic late Paleozoic Dniepr-Donets rift basin. It is situated in an intracratonic setting but close to the southern margin of the ...
TRACING TECTONIC DEFORMATION USING THE SEDIMENTARY RECORD: AN OVERVIEW

McCann T.; Saintot A. (2003)

Tectonic activity, on a range of scales, is a fundamental control on sedimentary activity. The range of structural deformation within a region extends from the plate tectonic scale, governing, for example, rift initiation, ...

Browsing ELibrary by Author "Saintot A."

Browsing ELibrary by Author "Saintot A."

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