Aarhus University Seal / Aarhus Universitets segl

Gry Barfod

Composition and origin of rhyolite melt intersected by drilling in the Krafla geothermal field, Iceland

Publikation: Bidrag til tidsskrift/Konferencebidrag i tidsskrift /Bidrag til avisTidsskriftartikelForskningpeer review

  • R. A. Zierenberg, Univ Calif Davis, University of California Davis, University of California System, Dept Geol, Ukendt
  • P. Schiffman, Univ Calif Davis, University of California Davis, University of California System, Dept Geol, USA
  • G. H. Barfod
  • Charles Lesher
  • N. E. Marks, Univ Calif Davis, University of California Davis, University of California System, Dept Geol, Ukendt
  • J. B. Lowenstern, US Geol Survey, United States Geological Survey, Ukendt
  • A. K. Mortensen, Iceland GeoSurvey ISOR, Danmark
  • E. C. Pope, Stanford Univ, Stanford University, Dept Geol & Environm Sci, USA
  • D. K. Bird, Stanford Univ, Stanford University, Dept Geol & Environm Sci, USA
  • M. H. Reed, 1272 Univ Oregon, Oregon University System, University of Oregon, Dept Geol Sci, Ukendt
  • G. O. Frioleifsson, HS Orka Hf, Ukendt
  • W. A. Elders, Univ Calif Riverside, University of California Riverside, University of California System, Dept Earth Sci, Ukendt

The Iceland Deep Drilling Project Well 1 was designed as a 4- to 5-km-deep exploration well with the goal of intercepting supercritical hydrothermal fluids in the Krafla geothermal field, Iceland. The well unexpectedly drilled into a high-silica (76.5 % SiO2) rhyolite melt at approximately 2.1 km. Some of the melt vesiculated while extruding into the drill hole, but most of the recovered cuttings are quenched sparsely phyric, vesicle-poor glass. The phenocryst assemblage is comprised of titanomagnetite, plagioclase, augite, and pigeonite. Compositional zoning in plagioclase and exsolution lamellae in augite and pigeonite record changing crystallization conditions as the melt migrated to its present depth of emplacement. The in situ temperature of the melt is estimated to be between 850 and 920 A degrees C based on two-pyroxene geothermometry and modeling of the crystallization sequence. Volatile content of the glass indicated partial degassing at an in situ pressure that is above hydrostatic (similar to 16 MPa) and below lithostatic (similar to 55 MPa). The major element and minor element composition of the melt are consistent with an origin by partial melting of hydrothermally altered basaltic crust at depth, similar to rhyolite erupted within the Krafla Caldera. Chondrite-normalized REE concentrations show strong light REE enrichment and relative flat patterns with negative Eu anomaly. Strontium isotope values (0.70328) are consistent with mantle-derived melt, but oxygen and hydrogen isotope values are depleted (3.1 and -118 aEuro degrees, respectively) relative to mantle values. The hydrogen isotope values overlap those of hydrothermal epidote from rocks altered by the meteoric-water-recharged Krafla geothermal system. The rhyolite melt was emplaced into and has reacted with a felsic intrusive suite that has nearly identical composition. The felsite is composed of quartz, alkali feldspar, plagioclase, titanomagnetite, and augite. Emplacement of the rhyolite magma has resulted in partial melting of the felsite, accompanied locally by partial assimilation. The interstitial melt in the felsite has similar normalized SiO2 content as the rhyolite melt but is distinguished by higher K2O and lower CaO and plots near the minimum melt composition in the granite system. Augite in the partially melted felsite has re-equilibrated to more calcic metamorphic compositions. Rare quenched glass fragments containing glomeroporphyritic crystals derived from the felsite show textural evidence for resorption of alkali feldspar and quartz. The glass in these fragments is enriched in SiO2 relative to the rhyolite melt or the interstitial felsite melt, consistent with the textural evidence for quartz dissolution. The quenching of these melts by drilling fluids at in situ conditions preserves details of the melt-wall rock interaction that would not be readily observed in rocks that had completely crystallized. However, these processes may be recognizable by a combination of textural analysis and in situ analytical techniques that document compositional heterogeneity due to partial melting and local assimilation.

OriginalsprogEngelsk
TidsskriftContributions to Mineralogy and Petrology
Vol/bind165
Nummer2
Sider (fra-til)327-347
Antal sider21
ISSN0010-7999
DOI
StatusUdgivet - feb. 2013
Eksternt udgivetJa

Se relationer på Aarhus Universitet Citationsformater

ID: 84126290