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Comparative field study of shallow rhyolite intrusions in Iceland : Emplacement mechanisms and impact on country rocks

Saubin, Elodie (författare)
Univ Canterbury, Dept Geol Sci, Ilam Rd, Christchurch 8041, New Zealand
Kennedy, Ben (författare)
Univ Canterbury, Dept Geol Sci, Ilam Rd, Christchurch 8041, New Zealand
Tuffen, Hugh (författare)
Univ Lancaster, Lancaster Environm Ctr, Lancaster, England
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Villeneuve, Marlene (författare)
Univ Canterbury, Dept Geol Sci, Ilam Rd, Christchurch 8041, New Zealand
Davidson, Jonathan (författare)
Univ Canterbury, Dept Geol Sci, Ilam Rd, Christchurch 8041, New Zealand
Burchardt, Steffi, 1982- (författare)
Uppsala universitet,Mineralogi, petrologi och tektonik
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 (creator_code:org_t)
ELSEVIER, 2019
2019
Engelska.
Ingår i: Journal of Volcanology and Geothermal Research. - : ELSEVIER. - 0377-0273 .- 1872-6097. ; 388
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Shallow silicic intrusions are known to exist in many active volcanoes and can fuel both eruptions and hydrothermal fields. However, our knowledge of magma intrusions remains far from complete, and processes occurring at intrusion margins are poorly understood. In this field-based study, we characterise four shallows, dissected rhyolitic intrusions at three sites in Iceland (Njarovik-Dyrfjoll, Krafla and Husafell central volcanoes). We focus on the relationship between intrusion emplacement mechanisms and country rock response, employing scanline mapping of fractures and in-situ rock property measurements (hardness and permeability) along transects from the intrusion margins to damaged and undamaged country rocks. We identify various scenarios of shallow intrusion emplacement style, based upon their diverse geometry and lithofacies architecture. Additional information from rock properties and characteristics of fractures and vesicles, indicates that initial country rock properties strongly influence the emplacement style. We identify two discrete types of country rock response to magma injection. The matrix permeability of weak, porous and permeable lithologies (conglomerate and hyaloclastite) is reduced by >1 order of magnitude adjacent to intrusions due to pore occlusion. Stronger and denser, low-permeability lithologies (basalt and welded ignimbrite) undergo a decrease in hardness by a factor >2 related to an up to fivefold increase in fracture density, with no significant change in matrix permeability. Our observations highlight the importance of robust characterisation of the mechanical properties of caldera-filling or geothermal reservoir formations, for appropriate forecasting of magma mobility, geophysical data interpretation, and geothermal resources characterisation.

Ämnesord

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

Nyckelord

Rhyolite
Intrusion
Iceland
Damage
Emplacement
Permeability

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