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LATE CRETACEOUS STRUCTURAL CONTROL AND ALPINE OVERPRINT OF THE HIGH-SULFIDATION CU–AU EPITHERMAL CHELOPECH DEPOSIT, SREDNOGORIE BELT, BULGARIA

Chambefort I.; Moritz R. (2006)

The Chelopech epithermal high-sulfidation deposit is located in the Panagyurishte ore district in Bulgaria, which is defined by a NNW alignment of Upper Cretaceous porphyry–Cu and Cu–Au epithermal deposits, and forms part ...

LATE CRETACEOUS TO EARLY PALEOGENE PALEOMAGNETIC RESULTS FROM SIKHOTE ALIN, FAR EASTERN RUSSIA: IMPLICATIONS FOR DEFORMATION OF EAST ASIA

Otofuji Y.i.; Shibata T.; Matsumoto M.; Yamamoto T.; Morimoto C.; Kulinich R.G.; Matsuda T.; Itaya T.; Zimin P.S.; Matunin A.P.; Sakhno V.G.; Kimura K. (1995)

Welded tuffs in the Bogopol and Sijanov groups were sampled at 27 sites from 12 caldera formations in the Sikhote Alin mountain range around Kavalerovo (44.3°N, 135.0°E) for chronological and paleomagnetic studies. KAr age ...

LATE CRETACEOUS-CENOZOIC DEFORMATION OF NORTHEAST ASIA

Gaina C.; Müller R.D.; Roest W.R. (2002)

The plate tectonic paradigm implies rigid plates and narrow plate boundaries. In contrast, diffuse plate boundaries are common both in the oceans and continents [R.G. Gordon, Annu. Rev. Earth Planet. Sci. 26 (1998) 615–642], ...

LATE CRETACEOUS-EARLY CENOZOIC TECTONIC EVOLUTION OF THE EURASIAN ACTIVE MARGIN IN THE CENTRAL AND EASTERN PONTIDES, NORTHERN TURKEY

Rice S.P.; Robertson A.H.F.; Ustaömer T. (2006)

The Izmir-Ankara-Erzincar suture zone (IAESZ) in the Central and the Eastern Pontides comprises a stack of thrust sheets of mainly Late Cretaceous-Early Cenozoic age that are restored as: (1) a subduction-accretion complex; ...

LATE DEVONIAN (FAMENNIAN) LUNGFISHES FROM THE CATSKILL FORMATION OF PENNSYLVANIA, USA

Friedman M.; Daeschler E.B. (2006)

Occurrences of fossil lungfishes (Dipnoi: Sarcopterygii) in the Famennian Catskill Formation of Pennsylvania are reviewed. A nearly complete dermal skull roof is assigned to a new genus and species, Apatorhynchus opistheretmus. ...

LATE DEVONIAN DIAMONDIFEROUS KIMBERLITE AND ALKALINE PICRITE (PROTO-KIMBERLITE?) MAGMATISM IN THE ARKHANGELSK REGION, NW RUSSIA

Mahotkin I.L.; Gibson S.A.; Thompson R.N.; Zhuravlev D.Z.; Zherdev P.U. (2000)

Widespread penecontemporaneous igneous activity affected NW Russia (the Kola Peninsula and adjoining areas to the SE around Arkhangelsk) during the Late Devonian (360–380 Ma). Magmatism varies from tholeiitic basalts, ...

LATE DEVONIAN GRANITE GNEISS COMPLEX OF THE SOUTHERN URALS

Degtyarev K.E.; Luchitskaya M.V.; Astrakhantsev O.V.; Shatagin K.N.; Sal'nikova E.B.; Kotov A.B. (2003)

Late Devonian is a crucial boundary in the evolution of the Uralian active margin of the East European Craton. This time is characterized by the beginning of collision of the East European continent with the Magnitogorsk ...

LATE DEVONIAN MAGMATISM IN THE PRIPYAT PALAEORIFT: A GEODYNAMIC MODEL

Aizberg R.Y.; Starchik T.A.; Beskopylny V.N.; Tsekoyeva T.K. (2001)

Late Devonian magmatism in the Pripyat Trough, Belarus was associated with the development of the intraplate Pripyat-Donets Palaeorift. Magmatic rocks belong to an alkali-ultrabasic-alkali-basaltoid suite. These are ...

LATE DEVONIAN PALEOGEOGRAPHY OF THE WEST SIBERIAN PLAIN AND ITS MOUNTAINOUS SURROUNDINGS

Yolkin E.A.; Bakharev N.K.; Izokh N.G.; Kirda N.P.; Kletz A.G.; Kontorovich V.A.; Obut O.T.; Timokhina I.G. (2003)

A Late Devonian paleogeographic reconstruction for the territory of the West Siberian Plate and the surrounding regions of the Altai-Sayan folded area and the Siberian Platform has been proposed. Zones of continental, ...

LATE EOCENE IMPACT EJECTA: GEOCHEMICAL AND ISOTOPIC CONNECTIONS WITH THE POPIGAI IMPACT STRUCTURE

Whitehead J.; Spray J.G.; Papanastassiou D.A.; Wasserburg G.J.; Grieve R.A.F. (2000)

Late Eocene microtektites and crystal-bearing microkrystites extracted from DSDP and ODP cores from the Atlantic, Pacific, and Indian oceans have been analyzed to address their provenance. A new analysis of Nd and Sr ...

Late Eocene impact ejecta: geochemical and isotopic connections with the Popigai impact structure.

Whitehead, J; Papanastassiou, D A; Spray, J G; Grieve, R A F; Wasserburg, Gerald J (PANGAEA, 2000-06-26)

LATE FRASNIAN-FAMENNIAN CLIMATES BASED ON PALYNOMORPH ANALYSES AND THE QUESTION OF THE LATE DEVONIAN GLACIATIONS

Streel M.; Caputo M.V.; Loboziak S.; Melo J.H.G. (2000)

Palynomorph distribution in Euramerica and western Gondwana, from the Latest Givetian to the Latest Famennian, may be explained, to some extent, by climatic changes. Detailed miospore stratigraphy dates accurately the ...

Late Glacial and Holocene changes in vegetation cover and climate in southern Siberia derived from a 15 kyr long pollen record from Lake Kotokel.

Tarasov, Pavel E; Bezrukova, Elena V; Krivonogov, Sergey K (PANGAEA, 2009-06-11)

In this study a radiocarbon-dated pollen record from Lake Kotokel (52°47' N, 108°07' E, 458 m a.s.l.) located in southern Siberia east of Lake Baikal was used to derive quantitative characteristics of regional vegetation ...

Late Glacial and Holocene environmental history on the eastern slope of the Middle Ural mountains, Russia.

Antipina, T G (PANGAEA, 2018-04-05)

Late Glacial and Holocene landscape dynamics in the southern taiga zone of East European Plain according to pollen and macrofossil records from the Central Forest State Reserve (Valdai Hills, Russia).

Novenko, Elena Y (PANGAEA, 2018-04-20)

LATE GLACIAL AND HOLOCENE VEGETATIONAL CHANGES ON THE ULAGAN HIGH-MOUNTAIN PLATEAU, ALTAI MOUNTAINS, SOUTHERN SIBERIA

Blyakharchuk T.A.; Wright H.E.; Borodavko P.S.; Knaap W.O.V.D.; Ammann B. (2004)

Three well-dated pollen diagrams from 1985 m, 2050 m, and at the tree line at 2150 m asl show the vegetational succession in the central Altai Mountains since 16 cal ka BP. Pioneer vegetation after deglaciation was recorded ...

LATE GLACIAL TO HOLOCENE BENTHIC FORAMINIFERA IN THE MARMARA SEA: IMPLICATIONS FOR BLACK SEA-MEDITERRANEAN SEA CONNECTIONS FOLLOWING THE LAST DEGLACIATION

Kaminski M.A.; Box M.; Filipescu S.; Al-Salameen M.; Aksu A.; Hiscott R.N. (2002)

Benthic foraminifera were studied from four gravity cores that penetrated Holocene marine sediments in the Marmara Sea. Morphogroup and assemblage analyses reveal that the Holocene sea-level rise did not result in a ...

Late Glacial to Holocene environments in the present-day coldest region of the Northern Hemisphere inferred from a pollen record of Lake Billyakh, Verkhoyansk Mts, NE Siberia.

Müller, Stefanie; Tarasov, Pavel E; Andreev, Andrei A; Diekmann, Bernhard (PANGAEA, 2008-11-28)

In this study a radiocarbon-dated pollen record from Lake Billyakh (65°17'N, 126°47'E; 340 m a.s.l.) in the Verkhoyansk Mountains was used to reconstruct vegetation and climate change since about 15 kyr BP (1 kyr=1000 cal. ...

Late Glacial to Holocene paleoenvironmental change on the northwestern Pacific seaboard, Kamchatka Peninsula (Russia)

Pendea Ionel Florin; Ponomareva Vera; Bourgeois Joanne; Zubrow Ezra B.W.; Portnyagin Maxim; Ponkratova Irina; Harmsen Hans; Korosec Gregory (2017)

We used a new sedimentary record from a small kettle wetland to reconstruct the Late Glacial and Holocene vegetation and fire history of the Krutoberegovo-Ust Kamchatsk region in eastern Kamchatka Peninsula (Russia). Pollen ...

LATE GLACIAL TO HOLOCENE PALEOENVIRONMENTAL EVOLUTION OF THE BLACK SEA, RECONSTRUCTED WITH STABLE OXYGEN ISOTOPE RECORDS OBTAINED ON OSTRACOD SHELLS

Bahr A.; Wefer G.; Arz H.W.; Lamy F. (2006)

High-resolution stable oxygen isotope (δ18O on ostracod shells), XRF-scanning and bulk grain-size data obtained on a transect of 6 gravity cores from the continental slope in the northwestern Black Sea give new insight ...

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