Sub-surface geology and velocity structure of the Krafla high temperature geothermal field, Iceland: Integrated ditch cuttings, wireline and zero offset vertical seismic profile analysis

Author:

Millett John M.ORCID,Planke Sverre,Kästner Felix,Blischke Anett,Hersir Gylfi Páll,Halldórsdóttir Sæunn,Flóvenz Ólafur G.,Árnadóttir Sigurveig,Helgadóttir Helga M.,Vakulenko Sergey,Buryak Sergey,Erlendsson Ögmundur,Giese Rüdiger,Cavailhes Jehanne P.,Jerram Dougal A.,Guðmundsson Ásgrímur,Júlíusson Egill

Funder

Seventh Framework Programme

Research Council of Norway

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference73 articles.

1. The development of volcanic sequences at rifted margins: new insights from the structure and morphology of the Vøring Escarpment, mid-Norwegian Margin;Abdelmalak;J. Geophys. Res. Solid Earth,2016

2. Mafic intrusions, hydrothermal venting, and the basalt-sediment transition: linking onshore and offshore examples from the North Atlantic igneous province;Angkasa;Interpretation,2017

3. Exploration and development of the Krafla geothermal area;Ármannsson;Jökull,1987

4. A study of the Krafla volcano using gravity, micro-earthquake and MT data;Árnason,2008

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