Magnetotelluric Image of Transcrustal Magmatic System Beneath the Tulu Moye Geothermal Prospect in the Ethiopian Rift

[1]  G. Natale,et al.  Caldera unrest driven by CO2-induced drying of the deep hydrothermal system , 2018, Scientific Reports.

[2]  Paul W. J. Glover,et al.  A modified Archie’s law for two conducting phases , 2000 .

[3]  Freysteinn Sigmundsson,et al.  Geophysical constraints on the dynamics of spreading centres from rifting episodes on land , 2012 .

[4]  Gylfi Páll Hersir,et al.  Joint 1D inversion of TEM and MT data and 3D inversion of MT data in the Hengill area, SW Iceland , 2010 .

[5]  G. Chiodini,et al.  Magmas near the critical degassing pressure drive volcanic unrest towards a critical state , 2016, Nature Communications.

[6]  Gary D. Egbert,et al.  3-D joint inversion of the magnetotelluric phase tensor and vertical magnetic transfer functions , 2015 .

[7]  Elias Lewi,et al.  Pulses of deformation reveal frequently recurring shallow magmatic activity beneath the Main Ethiopian Rift , 2011 .

[8]  E. Spangenberg,et al.  Effect of the water–steam phase transition on the electrical conductivity of porous rocks , 2010 .

[9]  Alan G. Jones,et al.  The magnetotelluric method : theory and practice , 2012 .

[10]  G. Jiracek Near-surface and topographic distortions in electromagnetic induction , 1990 .

[11]  H. Bibby,et al.  The magnetotelluric phase tensor , 2004 .

[12]  P. Wannamaker,et al.  Three‐dimensional electrical resistivity model of the hydrothermal system in Long Valley Caldera, California, from magnetotellurics , 2016 .

[13]  A. Pommier,et al.  "SIGMELTS": A web portal for electrical conductivity calculations in geosciences , 2010, Comput. Geosci..

[14]  Alexander V. Grayver,et al.  Parallel three-dimensional magnetotelluric inversion using adaptive finite-element method. Part I: theory and synthetic study , 2015 .

[15]  A. Jackson,et al.  3-D analysis and interpretation of magnetotelluric data from the Aluto-Langano geothermal field, Ethiopia , 2015 .

[16]  F. Salvini,et al.  Elliptic calderas in the Ethiopian Rift: control of pre-existing structures , 2003 .

[17]  C. Ebinger,et al.  Volcanism in the Afar Rift sustained by decompression melting with minimal plume influence , 2012 .

[18]  S. Buiter,et al.  Complex fault interaction controls continental rifting , 2017, Nature Communications.

[19]  F. Sigmundsson,et al.  The role of smectites in the electrical conductivity of active hydrothermal systems: electrical properties of core samples from Krafla volcano, Iceland , 2018, Geophysical Journal International.

[20]  H. Behrens,et al.  Probing the status of felsic magma reservoirs: Constraints from the P-T-H 2 O dependences of electrical conductivity of rhyolitic melt , 2016 .

[21]  C. Deniel,et al.  Crustal control in the genesis of Plio-Quaternary bimodal magmatism of the Main Ethiopian Rift (MER): geochemical and isotopic (Sr, Nd, Pb) evidence , 1999 .

[22]  G. Yirgu,et al.  Constraining magma storage conditions at a restless volcano in the Main Ethiopian Rift using phase equilibria models , 2017 .

[23]  R. Groom,et al.  Corrections for near surface effects: Decomposition of the magnetotelluric impedance tensor and scaling corrections for regional resistivities: A tutorial , 1992 .

[24]  E. Rivalta,et al.  Off-rift volcanism in rift zones determined by crustal unloading , 2014 .

[25]  Vladimir I. Dmitriev,et al.  Models and Methods of Magnetotellurics , 2008 .

[26]  C. Ebinger,et al.  Magma-assisted rifting in Ethiopia , 2005, Nature.

[27]  R. Sparks,et al.  Vertically extensive and unstable magmatic systems: A unified view of igneous processes , 2017, Science.

[28]  R. C. Bailey,et al.  Decomposition of magnetotelluric impedance tensors in the presence of local three-dimensional galvanic distortion , 1989 .

[29]  A. Grayver,et al.  Topographic distortions of magnetotelluric transfer functions: a high-resolution 3-D modelling study using real elevation data , 2018, Geophysical Journal International.

[30]  Michele Manunta,et al.  SBAS-DInSAR Parallel Processing for Deformation Time-Series Computation , 2014, IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing.

[31]  S. Tait,et al.  Measurements of the evolution of porosity in a mushy layer , 1996 .

[32]  G. Corti,et al.  Continental rift evolution: From rift initiation to incipient break-up in the Main Ethiopian Rift, East Africa , 2009 .

[33]  Rebecca Bendick,et al.  GPS constraints on broad scale extension in the Ethiopian Highlands and Main Ethiopian Rift , 2016 .

[34]  Adele Manzella,et al.  Electromagnetic sounding of geothermal zones , 2009 .

[35]  S. Hautot,et al.  A mantle magma reservoir beneath an incipient mid-ocean ridge in Afar, Ethiopia , 2013 .

[36]  G. Wadge,et al.  Historical Volcanism and the State of Stress in the East African Rift System , 2016, Front. Earth Sci..

[37]  C. Ebinger,et al.  Strain accommodation by magmatism and faulting as rifting proceeds to breakup: Seismicity of the northern Ethiopian rift , 2006 .

[38]  S. Constable,et al.  Electrical image of passive mantle upwelling beneath the northern East Pacific Rise , 2013, Nature.

[39]  S. Hautot,et al.  Magma imaged magnetotellurically beneath an active and an inactive magmatic segment in Afar, Ethiopia , 2015, Special Publications.

[40]  Paul L. Younger,et al.  Missing a trick in geothermal exploration , 2014 .

[41]  É. Calais,et al.  Dual continental rift systems generated by plume-lithosphere interaction , 2015 .