Geochemistry of high-temperature granulitic supracrustals from Rogaland, SW Norway

L.C.G.M. Bol

Geochemistry of high-temperature granulitic supracrustals from Rogaland, SW Norway

L.C.G.M. Bol

Research Programme in Earth Sciences Utrecht (DES / IVAU)

Research output: Thesis › Doctoral thesis 1 (Research UU / Graduation UU)

Abstract

Were the granulite-facies metamorphic supracrustals of the Faurefjell Metasediment Formation in Rogaland, SW Norway, chemically open or closed systems? In order to assess differential element mobilities in response to pre-, syn- and post-metamorphic fluid fluxes through this formation, the mineralogy, crystal chemistry, bulk chemical composition, and mineral oxygen and carbon stable isotope composition is investigated in marbles and metavolcanics.

Original language	English
Qualification	Doctor of Philosophy
Awarding Institution	Utrecht University
Supervisors/Advisors	Schuiling, R.D., Primary supervisor Jansen, J.B.H., Co-supervisor, External person
Award date	11 Jun 1990
Place of Publication	Utrecht
Publisher	Faculteit Aardwetenschappen
Print ISBNs	90-71577-19-8
Publication status	Published - 11 Jun 1990

Bibliographical note

Geologica Ultraiectina ; 66

Keywords

granulite
geochemistry
Rogaland fylke
Norway
metamorphic petrology
stable isotopes

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Bol-Luc CGM-66-1990Final published version, 6.72 MB

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title = "Geochemistry of high-temperature granulitic supracrustals from Rogaland, SW Norway",

abstract = "Were the granulite-facies metamorphic supracrustals of the Faurefjell Metasediment Formation in Rogaland, SW Norway, chemically open or closed systems? In order to assess differential element mobilities in response to pre-, syn- and post-metamorphic fluid fluxes through this formation, the mineralogy, crystal chemistry, bulk chemical composition, and mineral oxygen and carbon stable isotope composition is investigated in marbles and metavolcanics.",

keywords = "granulite, geochemistry, Rogaland fylke, Norway, metamorphic petrology, stable isotopes",

author = "L.C.G.M. Bol",

note = "Geologica Ultraiectina ; 66 ",

year = "1990",

month = jun,

day = "11",

language = "English",

isbn = "90-71577-19-8",

publisher = "Faculteit Aardwetenschappen",

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T1 - Geochemistry of high-temperature granulitic supracrustals from Rogaland, SW Norway

AU - Bol, L.C.G.M.

N1 - Geologica Ultraiectina ; 66

PY - 1990/6/11

Y1 - 1990/6/11

N2 - Were the granulite-facies metamorphic supracrustals of the Faurefjell Metasediment Formation in Rogaland, SW Norway, chemically open or closed systems? In order to assess differential element mobilities in response to pre-, syn- and post-metamorphic fluid fluxes through this formation, the mineralogy, crystal chemistry, bulk chemical composition, and mineral oxygen and carbon stable isotope composition is investigated in marbles and metavolcanics.

AB - Were the granulite-facies metamorphic supracrustals of the Faurefjell Metasediment Formation in Rogaland, SW Norway, chemically open or closed systems? In order to assess differential element mobilities in response to pre-, syn- and post-metamorphic fluid fluxes through this formation, the mineralogy, crystal chemistry, bulk chemical composition, and mineral oxygen and carbon stable isotope composition is investigated in marbles and metavolcanics.

KW - granulite

KW - geochemistry

KW - Rogaland fylke

KW - Norway

KW - metamorphic petrology

KW - stable isotopes

M3 - Doctoral thesis 1 (Research UU / Graduation UU)

SN - 90-71577-19-8

PB - Faculteit Aardwetenschappen

CY - Utrecht

ER -

Geochemistry of high-temperature granulitic supracrustals from Rogaland, SW Norway

Abstract

Bibliographical note

Keywords

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Cite this