Results 121 to 130 of about 343 (176)

The origin, source, and cycling of methane in deep crystalline rock biosphere. [PDF]

Front Microbiol, 2015
Kietäväinen R, Purkamo L.
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Toxigenic Cyanobacteria and Microcystins in a Large Northern Oligotrophic Lake Onego, Russia. [PDF]

Toxins (Basel)
Tekanova E, Sidelev S, Kalinkina N, Chernova E, Barinova S, Sharov A, Smirnova V.   +6 more
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Mobility and community at Mesolithic Lake Onega, Karelia, north-west Russia: insights from strontium isotope analysis. [PDF]

Archaeol Anthropol Sci
Eckelmann R, Arppe L, Tarasov A, Pospieszny Ł, Ackerman L, Heyd V, Gerasimov D, Moiseyev V, Fairbanks V, Hyland C, Mannermaa K.   +10 more
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Geographic differences in lung cancer: focus on carcinogens, genetic predisposition, and molecular epidemiology. [PDF]

Ther Adv Med Oncol
Laguna JC, García-Pardo M, Alessi J, Barrios C, Singh N, Al-Shamsi HO, Loong H, Ferriol M, Recondo G, Mezquita L.   +9 more
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Bear in mind! Bear presence and individual experience with calf survival shape the selection of calving sites in a long-lived solitary ungulate. [PDF]

Ecol Evol
Dijkgraaf L, Stenbacka F, Cromsigt JPGM, Ericsson G, Neumann W.   +4 more
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Radiolytic support for oxidative metabolism in an ancient subsurface brine system. [PDF]

ISME Commun
Nisson DM, Kieft TL, Castillo J, Perl SM, Onstott TC.   +4 more
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Recognition of low-temperature processes in the Fennoscandian shield

, 1997
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SEISMIC ZONING OF FENNOSCANDIAN SHIELD

ISET Journal of Earthquake Technology, 1974
The major earthquake zones of the world are found in (i) the Circum-Pacific belt, (ii) the Alpine-Himalayan belt and (iii)the mid-oceanic ridges of the Atlantic, Indian and Pacific oceans. These earthquake-belts which cover large segments of the Earth, have been studied in detail by various workers, but little attention has been paid to earthquake ...
L. S. SRIVASTAVA, M. A. SELLEVOLL
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Metallogeny of gold in the Fennoscandian Shield

Mineralium Deposita, 1990
Gold occurs in a number of different ore types in the Fennoscandian Shield ranging in age from Late Archean to Late Proterozoic. Until recently, the metal was exploited primarily as a byproduct in volcanogenic massive sulphide deposits but during the 1980s more gold mines have been opened than during any other episode in the mining history of northern ...
G. Gaál, K. Sundblad
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The Archaean nucleus of the Fennoscandian (Baltic) Shield

Geological Society, London, Memoirs, 2006
abstract Archaean supracrustal complexes, known in the Fennoscandian (Baltic) Shield, are described and discussed by analysing the time sections 3.1-2.9, 2.9-2.75 and 2.75-2.65 Ga. Data on granitoid complexes, interrelated in time and space, and evidence for Archaean metamorphic events are classified and presented briefly.
A. I. Slabunov, S. B. Lobach-Zhuchenko, E. V. Bibikova, P. Sorjonen-Ward, V. V. Balangansky, O. I. Volodichev, A. A. Shchipansky, S. A. Svetov, V. P. Chekulaev, N. A. Arestova, V. S. Stepanov   +10 more
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