Endre søk
RefereraExporteraLink to record
Permanent link

Direct link
Referera
Referensformat
  • apa
  • harvard1
  • ieee
  • modern-language-association-8th-edition
  • vancouver
  • Annet format
Fler format
Språk
  • de-DE
  • en-GB
  • en-US
  • fi-FI
  • nn-NO
  • nn-NB
  • sv-SE
  • Annet språk
Fler språk
Utmatningsformat
  • html
  • text
  • asciidoc
  • rtf
Geochemical characteristics of granites associated with Proterozoic molybdenite mineralization in northern Sweden
Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser, Geovetenskap och miljöteknik.
1985 (engelsk)Inngår i: Chemical Geology, ISSN 0009-2541, E-ISSN 1872-6836, Vol. 51, nr 3-4, s. 247-263Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

Proterozoic molybdenite occurrences in northern Sweden are associated with small plutons of intrusive character located in supracrustal belts whereas large granite areas are barren. In this study, 152 samples of granites associated with molybdenite mineralization, mineralized aplites, granites not known to be associated with molybdenite occurrences but located in supracrustal belts and granites from the large granite areas have been analysed for major elements and the selected trace elements Mo, Sn, Be, Ba, Rb, Sr, Cu, Zn, Zr, V, Y, Nb, F, Cl and S. The study showed that major-element geochemistry and modal composition are not useful for distinguishing between potentially molybdenite-mineralizing and barren granites in northern Sweden. Enriched contents of Sn, Be, Y, Rb and F are most useful for identifying ore-associated granites in the supracrustal belts. The granites from the large granite areas have very low contents of Sn, Mo, Be, Nb, Y, F, Cl and S. It is proposed that the granites associated with molybdenite occurrences were probably generated by partial melting of earlier igneous rocks, or they may be of subcrustal origin, the large granite bodies originated by partial melting of Archean continental crust.

sted, utgiver, år, opplag, sider
1985. Vol. 51, nr 3-4, s. 247-263
HSV kategori
Forskningsprogram
Tillämpad geologi
Identifikatorer
URN: urn:nbn:se:ltu:diva-8079DOI: 10.1016/0009-2541(85)90136-6ISI: A1985AVL6400008Scopus ID: 2-s2.0-0022167875Lokal ID: 684c2920-e548-11dc-bcb4-000ea68e967bOAI: oai:DiVA.org:ltu-8079DiVA, id: diva2:980969
Merknad
Godkänd; 1985; 20080227 (ysko)Tilgjengelig fra: 2016-09-29 Laget: 2016-09-29 Sist oppdatert: 2018-07-10bibliografisk kontrollert

Open Access i DiVA

Fulltekst mangler i DiVA

Andre lenker

Forlagets fulltekstScopus

Personposter BETA

Öhlander, Björn

Søk i DiVA

Av forfatter/redaktør
Öhlander, Björn
Av organisasjonen
I samme tidsskrift
Chemical Geology

Søk utenfor DiVA

GoogleGoogle Scholar

doi
urn-nbn

Altmetric

doi
urn-nbn
Totalt: 18 treff
RefereraExporteraLink to record
Permanent link

Direct link
Referera
Referensformat
  • apa
  • harvard1
  • ieee
  • modern-language-association-8th-edition
  • vancouver
  • Annet format
Fler format
Språk
  • de-DE
  • en-GB
  • en-US
  • fi-FI
  • nn-NO
  • nn-NB
  • sv-SE
  • Annet språk
Fler språk
Utmatningsformat
  • html
  • text
  • asciidoc
  • rtf