Facies analysis of the Breidavík Group sediments on Tjörnes, north Iceland
Read Online
Share

Facies analysis of the Breidavík Group sediments on Tjörnes, north Iceland by JoМЃn EiriМЃksson.

  • 626 Want to read
  • ·
  • 16 Currently reading

Published by Iceland Museum of Natural History in Reykjavík .
Written in English

Subjects:

Places:

  • Breidavík Group (Iceland),
  • Iceland,
  • Tjörnes Peninsula.

Subjects:

  • Geology, Stratigraphic -- Quaternary.,
  • Geology -- Iceland -- Tjörnes Peninsula.,
  • Sediments (Geology) -- Iceland -- Tjörnes Peninsula.,
  • Breidavík Group (Iceland)

Book details:

Edition Notes

StatementJón Eiríksson.
SeriesActa naturalia Islandica,, 31
Classifications
LC ClassificationsQH166 .A75 no. 31, QE696 .A75 no. 31
The Physical Object
Pagination56 p. :
Number of Pages56
ID Numbers
Open LibraryOL2341391M
LC Control Number86234434

Download Facies analysis of the Breidavík Group sediments on Tjörnes, north Iceland

PDF EPUB FB2 MOBI RTF

Benvenuti A., Moscariello A. () Seismic Geometry and Facies Analysis of a Quaternary Tunnel Glacial Valley Infill in the Dutch North Sea: Preliminary Results. In: Rocha R., Pais J., Kullberg J., Finney S. (eds) STRATI Cited by: 1. Detailed facies analysis of the Balta Fm. of Ukraine, Moldova and Romania • Reveals a large Late Miocene fluvio-deltaic system in the East Carpathian foreland • Highlights the crucial final stage in the sedimentary evolution of the foreland basin • The extent of the East Carpathian foreland basin is proven to reach by: 9. Kristín Björg Ólafsdóttir, , Time series analyses based on paleoclimatic proxies from lake sediments in Iceland, Master‟s thesis, Faculty of Earth Sciences, University of Iceland, pp. ISBN XX Printing: Háskólaprent ehf. Reykjavik, Iceland, February Cited by: 2. The Jökulsá á Fjöllum flows northwards from the Vatnajökull icecap into the Arctic Ocean (Fig. 1A).It is km long, with its sources being meltwater streams that drain the margins of Dyngujökull and Kverkjökull glaciers (Fig. 1B), and a major tributary, the Kreppa, which drains the western portion of Brúarjökull.Jökulhlaups generated by the Barðabunga volcanic system have Cited by:

  We have developed the concept of microseismic facies analysis, a method that facilitates partitioning of an unconventional reservoir into distinct facies units on the basis of their microseismic response along with integrated interpretation of microseismic observations with 3D seismic data. It is based upon proposed links between magnitude-frequency distributions and Cited by: 9. NORWEGIAN JOURNAL OF GEOLOGY Depositional facies and reservoir quality 75 Fig. 5. Petrology of Facies A with grain size distribution and total clay content. Curves in upper right corners show the cumulative frequency of grain size and total clay content, separated by the subfacies A1, A2 and Size: KB. sediments in the uppermost part of the Tjornes sequence, North Iceland. However, there have been conflicting views on the stratigraphical position andnumberof glacial horizons, and on the significance of glacial signs in the sequence. Pjetursson () described two lithified "moraine" horizons separated by marine beds. Abstract. A detailed study of paleoclimatic proxy data (stable isotopes, planktonic foraminiferal census data, carbonate content, and Ice Rafted Detritus (IRD)) in the surface sediments of the Greenland, Iceland and Norwegian Seas (GIN-seas) shows that different proxies are closely related to the surface water masses, to the position of oceanic fronts and to the sea ice by:

ation of the sediments at this distinctive new type of vent field and focus mainly on the hydrothermal phyllosilicates. 2. Geologic Setting [4] The Grimsey vent field is situated east of Grimsey Island, SL km north of Iceland (Figure 1). It lies in the Grimsey Graben, a sediment-filled (buried to an average. Facies () – DOI /s ORIGINAL ARTICLE Facies arrangement and cyclostratigraphic architecture of a shallow-marine, warm-water carbonate platform: the Late Carboniferous Ny Friesland Platform in eastern Spitsbergen (Pyefjellet Beds, Wordiekammen Formation, Gipsdalen Group). This long and extensive history of thin-section analysis of glacigenic sediments has given rise to a set of well-defined criteria, summarised in Table 1. A combination of processes Recently, several researchers have argued that processes at the ice-bed interface are a result of a continuum of processes, including melt-out, lodgement.   The mid-Jurassic Garn Formation in the Halten Terrace area, Mid-Norway Continental Shelf, has been studied on the basis of ~ m of well-core samples from 9 selected wells, geophysical wireline logs from nearly 30 wide Author: Kay Sørbø.