SwePub
Sök i LIBRIS databas

  Extended search

onr:"swepub:oai:DiVA.org:uu-356330"
 

Search: onr:"swepub:oai:DiVA.org:uu-356330" > Sedimentology of th...

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

Sedimentology of the Lower Ordovician (upper Tremadocian) Bjørkasholmen Formation at Flagabro, southern Sweden

Egenhoff, Sven (author)
Colorado State Univ, Dept Geosci, Ft Collins, CO 80523 USA,Colorado State University
Maletz, Jörg (author)
Free Univ Berlin, Inst Geowissensch, Berlin, Germany,Free University of Berlin
Ahlberg, Per (author)
Lund University,Lunds universitet,Geologiska institutionen,Naturvetenskapliga fakulteten,Department of Geology,Faculty of Science
show more...
Mast, Allison (author)
Colorado State Univ, Dept Geosci, Ft Collins, CO 80523 USA,Colorado State University
Frisk, Åsa (author)
Uppsala University,Uppsala universitet,Evolutionsmuseet
Ebbestad, Jan Ove R., 1967- (author)
Uppsala University,Uppsala universitet,Evolutionsmuseet
Newby, Warren (author)
Colorado State Univ, Dept Geosci, Ft Collins, CO 80523 USA;Total Oil & Gas, Houston, TX 77010 USA,Colorado State University
show less...
 (creator_code:org_t)
2018-05-14
2018
English.
In: GFF. - : TAYLOR & FRANCIS LTD. - 1103-5897 .- 2000-0863. ; 140:1, s. 55-65
  • Journal article (peer-reviewed)
Abstract Subject headings
Close  
  • The Lower Ordovician Bjørkasholmen Formation at Flagabro, Scania, southern Sweden, consists of a 0.8m thick succession of carbonates with three siliciclastic mudstones, 5, 1 and 100mm thick, intercalated in the central part of the unit. Carbonate and siliciclastic mudstone beds show both normal and inverse grading. The carbonates are mud-rich and subdivided into a mudstone, a wackestone and a packstone facies. Grain types in the carbonates are mostly shells and shell fragments of brachiopods and trilobites. The carbonate rocks are strongly bioturbated seen as in roundish burrows filled with mud and a clear cement; additionally, bioturbation is reflected in the random orientation of shells. The siliciclastic mudstones are subdivided into two facies; one contains large amounts of shells and is in part grain-supported, the other is matrix-dominated and laminated to massive. The succession reflects sedimentation on a low-inclined shelf equivalent to a mid-ramp to basinal setting. Most mud- and wackestones (facies 3 and 4) represent fair-weather sedimentation, and the intercalated wacke- and packstones (facies 4 and 5) represent concentration of shell debris during high-energy storm. The siliciclastic mudstones in the central part of the succession reflect deposition in a basinal setting. The entire BjOrkasholmen Formation at Flagabro is equivalent to a lowstand of third (?) order without a well-developed internal cyclicity and is in that respect similar to the Bjørkasholmen Formation of oland, but different from the age-equivalent Norwegian sections.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)

Keyword

Bjørkasholmen Formation
carbonates
siliciclastic mudstones
Flagabro
Bjørkåsholmen Formation
carbonates
Flagabro
siliciclastic mudstones

Publication and Content Type

ref (subject category)
art (subject category)

Find in a library

  • GFF (Search for host publication in LIBRIS)

To the university's database

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

Search outside SwePub

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Close

Copy and save the link in order to return to this view