Monographie der arktischen Acariden /

Blank leaves bound between each leaf.

Norske ordsprog...

Mode of access: Internet.

Eusebius Werke /

Original Greek texts, some supplemented or accompanied by Latin versions; texts preserved in other languages, and editorial matter, in German.

Register til en del Norske tidsskrifter.

Vol. 1 mainly compiled by Ivar Sæter; edited by Arne Arnesen. cf. Pref.

Rococonoveller.

Mode of access: Internet.

Industri- och slöjdutställningen i Gefle 1901 : officiell berättelse /

Includes one folded map.

Ortnamnen i Älvsborgs län.

Issued in 25 pts. Pt. 1: Inledning, by Ivar Lundahl, issued by Kungl. Ortnamnskommissionen; pts. 2-25, by Kungl. Ortnamnskommittén.

Samlede værker /

Bd. 1. Arne. Synnøve Sølbakken. En glad gut. Jærnbanen og kirkegården. -- Bd. 2. Fiskerjænten. Brudeslåtten. Småstykker. Kaptejn Mansana. -- Bd. 3. Magnhild. Støv. Mors Hænder. Én dag. Et styggt barndomsminne. Ivar Bye. Absalons hår. -- Bd. 4. Det flager i byen og på havnen. -- Bd. 5. På Guds veje. Mary. -- Bd. 6. Mellem slagene. Halte-Hulda. Sigurd Slembe. Maria Stuart. Sigurd Jorsalfar. -- Bd. 7. De nygifte. Redaktøren. En fallit. Kongen. Leonarda. Det ny system. -- Bd. 8. Over ævne I-II. Geografi og kjærlighed. Paul Lange og Tora Parsberg. En hanske. -- Bd. 9. Laboremus. På Storhove. Daglannet. Når den ny vin blomstrer. -- Bd. 10. Digte og sange. Arnljot Gelline. Lyset.

La Galerie de tableaux de la Reine Christine de Suéde ayant appartenu anparavent à l'Enpersur Rodolphe II, plus tard aux ducs d'Orléans. Recherche historique et critique par ...

Mode of access: Internet.

(Table) Grain size distribution of sediments from core Ak-509, Black Sea continental slope

New results of geomorphological, seismoacoustic, and lithological investigations on the upper continental slope off the Arkhipo-Osipovka Settlement are presented. Here, a large submarine slump was discovered by seismic survey in 1998. The assumed slump body, up to 200 m thick, rises 50-60 m above the valley floor that cuts the slope. Recent semiliquid mud that overlies laminated slope sediments with possible slump deformations flows down in the valley thalweg. Radiocarbon age inversion recorded in a Holocene sediment section of shelf facies recovered from the upper slope points to the gravity dislocation of sediments.

Chemical and mineral composition of rocks from the Philippine Sea

The book is devoted to geology of the Philippine Sea floor. This region is studied most extensively among other marginal seas of the Pacific Ocean. Rocks of the sedimentary and basalt layers within this sea have been studied during five legs of D/S Glomar Challenger. International geological expedition on board R/V Dmitry Mendeleev carried out according to the Project ''Ophiolites of Continents and Comparable Rocks of the Ocean Floor''obtained unique collection of rocks from the second and third layers of the ocean crust in the Philippine Sea. The book provides detailed petrographic and geochemical description of igneous and sedimentary formations from the Philippine Sea and compares them with rocks of the continental ophiolite association. An analysis of structure and history of the ocean crust formation in the region is based on all known geological information. The main periods of tectonic movement activation and nature of their manifestations within the sea are shown.

(Table 1) Mineral composition of sand- and silt-sized fractions of bottom sediments from the Romanche Trench

A study was made of mineral composition of sand- and silt-sized fractions of recent clastic (riftogenic) sediments and solidified deposits collected from the bottom of the Romanche Trench during the first voyage of R/V Akademik Kurchatov. Similarity between mineral compositions of sediments and bedrocks (ultrabasites, gabbroids, diabases) was established. This similarity is a basis for considering the mineral complex of the deposits that have been derived from the bedrocks of the trench slopes, and have formed due to their submarine denudation accompanied by tectonic crushing. The same mineral composition was found in pieces of older consolidated deposits; this suggests that conditions of sedimentation similar to those at recent times have existed for a long time in the Romanche Trench.

Coarse-silt-fraction mineralogy at DSDP Legs 56 and 57 Holes

Soviet sedimentologists use the term "coarse silt" to denote the size fraction 0.1 to 0.05 mm (50-100 µm). Petelin (1961) has shown that this fraction is most diagnostic for terrigeneous and volcanogenic mineral assemblages and provinces in Recent deep-sea sediments, because of its greatest variability of both heavy and light non-opaque minerals, which may be easily identified by the common immersion method. We believe that the fraction is suitable for mineralogical study of unconsolidated and friable sediments from DSDP cores as well, if the objective is to investigate their source area and transporation tracks. In the case of fine-grained oceanic sediments, mineral composition of the coarse silt does not differ markedly from that of the "coarse fraction" (>62 µm).

Geochemistry of the Japan Trench sediments at DSDP Legs 56-57 Holes

The main objective of this investigation was to study distribution of main chemical constituents and several minor elements in sediment sections drilled during DSDP Legs 56 and 57 in the Japan Trench, in order to infer geochemical features of different lithologic types of sediments, and to find out how the geochemistry is associated with major lithologic constituents, such as terrigenous detrital matter, clay, volcanic ash, and biogenic particles. The geochemical data may help to indicate the nature of the sediments and to interpret sedimentation processes. The analyzed samples seem to be representative of most lithologic units, sub-units, and sediment types drilled at all sites on both legs, except for some shallow-water deposits at Sites 438 and 439. We analyzed bulk-sediment composition by X-ray fluorescence (Kuzmina and Turanskaya) and routine wet-chemical methods (Mikhailov); amorphous SiO2, extracted in a boiling sodium carbonate solution (Analythical Laboratory, P. P. Shirshov Institute of Oceanology); Cr, Zn, Cu, Ni, Co, and Al by atomic absorption (Gordeev); and Sn, Pb, Zn, Cu, Ni, Co, Cr, V, B, and Ag by quantitative spectrographic analyses in both bulk samples and granulometric fractions (Mikhailov). In addition, Fe, Ti, Mn, and CaCO3 have been determined in selected samples by routine wet-chemical methods (Analytical Laboratory, P. P. Shirshov Institute of Oceanology). Murdmaa was responsible for interpretation of the results.