Browsing ELibrary by Author "Filatova N.I."

Now showing items 1-8 of 8

CENOZOIC MAGMATISM HETEROGENEITY IN CONTINENTAL-MARGIN EXTENSION ZONES OF THE KOREAN PENINSULA: A POSSIBLE EXPLANATION

Fedorov P.I.; Filatova N.I. (2001)
COMPARATIVE SYSTEMATICS OF BASALTOIDS FROM THE EXTENSION ZONES OF THE ASIAN CONTINENTAL MARGIN AND THE OCEANIC ISLANDS OF THE PACIFIC OCEAN: ISOTOPIC AND SEISMIC TOMOGRAPHIC PERSPECTIVES

Filatova N.I. (2002)

Comparison of the Sr-Nd-Pb isotopic characteristics of the Cenozoic extension zone basalts (MEZB) of the Eurasian margin and the Cretaceous-Cenozoic OIB of the southern Pacific isotopic and thermal anomaly (SOPITA) ...
CORRELATION OF UPPER MESOZOIC SEDIMENTARY AND VOLCANOGENIC DEPOSITS OF KOREA AND THEIR DEPOSITIONAL SETTINGS

Filatova N.I.; Chang K.Kh.; Park S.O. (1999)

The Upper Mesozoic deposits of the northern and southern parts of the Korean Peninsula significantly differ from each other. The Upper Jurassic-Neocomian deposits of North Korea are represented by the differentiated volcanics ...
CRETACEOUS EVOLUTION OF CONTINENTAL MARGINS AS RELATED TO GLOBAL EVENTS

Filatova N.I. (1998)

The character and intensity of Cretaceous events in continental margins are genetically linked with the rate of oceanic crust accretion and intensity of endogenic (plume) activity of the Earth. This is most evidently proved ...
PALEOGEOGRAPHY OF THE BERRIASIAN-BARREMIAN AGES OF THE EARLY CRETACEOUS

Zharkov M.A.; Murdmaa I.O.; Filatova N.I. (1998)

Global litholologic-paleogeographic maps are compiled for the Berriasian, Valanginian, Hauterivian, and Barremian ages of the Early Cretaceous. Main features of paleogeography, sedimentation environments in oceans, ...
PALEOGEOGRAPHY OF THE CONIACIAN-MAASTRICHTIAN AGES OF THE LATE CRETACEOUS

Zharkov M.A.; Murdmaa I.O.; Filatova N.I. (1998)

Global lithologic-paleogeographic maps were compiled for the Coniacian, Santonian, Campanian, and Maastrichtian ages of the Late Cretaceous. Main features of paleogeography of continental and oceanic hemispheres of the ...
STRUCTURE AND GEODYNAMICS OF FORMATION OF ACTIVE CONTINENTAL MARGINS

Bogdanov N.A.; Filatova N.I. (2001)

The structure of active continental margins is characterized by development of volcanic and terrane fold-and-nappe orogenic belts, which collectively ensure the growth of continental margins both in area and crustal ...
UNDERPLATING AS A CAUSE OF THE VOLCANIC CONTINENTAL MARGIN FORMATION DURING MARGINAL SEA SPREADING

Filatova N.I. (2004)

Problems related to the rifting zones and continental margins of the opening sea basins include the necessity of explaining the alternation of active magmatic and a magmatic segments of continental margins recognized as ...

Browsing ELibrary by Author "Filatova N.I."

Browsing ELibrary by Author "Filatova N.I."

Search DSpace

Browse

All of DSpace

This Collection

My Account