Regional two-dimensional magnetotelluric profile in West Bohemia/Vogtland reveals deep conductive channel into the earthquake swarm region
暂无分享,去创建一个
[1] H. Kämpf,et al. Reconnaissance study of an inferred Quaternary maar structure in the western part of the Bohemian Massif near Neualbenreuth, NE-Bavaria (Germany) , 2018, International Journal of Earth Sciences.
[2] P. Hrubcová,et al. Active Magmatic Underplating in Western Eger Rift, Central Europe , 2017 .
[3] J. Plomerová,et al. Lateral displacement of crustal units relative to underlying mantle lithosphere: Example from the Bohemian Massif , 2017 .
[4] M. Alawi,et al. Drilling into an active mofette: pilot-hole study of the impact of CO 2 -rich mantle-derived fluids on the geo–bio interaction in the western Eger Rift (Czech Republic) , 2017 .
[5] C. Matyska,et al. Earthquake-enhanced permeability - evidence from carbon dioxide release following the M L 3.5 earthquake in West Bohemia , 2017 .
[6] C. Haberland,et al. Attenuation tomography in West Bohemia/Vogtland , 2017 .
[7] N. Meqbel,et al. Crustal metamorphic fluid flux beneath the Dead Sea Basin: constraints from 2-D and 3-D magnetotelluric modelling , 2016 .
[8] Kerry Key,et al. MARE2DEM: a 2-D inversion code for controlled-source electromagnetic and magnetotelluric data , 2016 .
[9] S. Hainzl,et al. Aftershocks triggered by fluid intrusion: Evidence for the aftershock sequence occurred 2014 in West Bohemia/Vogtland , 2016 .
[10] M. D. Wit,et al. A deep electrical conductivity structure of the southern Barberton Greenstone Belt, South Africa, derived from magnetotelluric measurements , 2016 .
[11] B. Růžek,et al. Origin of earthquake swarms in the western Bohemian Massif: Is the mantle CO2 degassing, followed by the Cheb Basin subsidence, an essential driving force? , 2016 .
[12] M. Korn,et al. Seismic tomography reveals a mid-crustal intrusive body, fluid pathways and their relation to the earthquake swarms in West Bohemia/Vogtland , 2015 .
[13] V. R. Gajevskiy. Electric Conductivity of Carbon Dioxide Aqueous Solutions , 2015 .
[14] H. Kämpf,et al. CO2 degassing in the Hartoušov mofette area, western Eger Rift, imaged by CO2 mapping and geoelectrical and gravity surveys , 2015, International Journal of Earth Sciences.
[15] K. Bräuer,et al. Seismically triggered anomalies in the isotope signatures of mantle‐derived gases detected at degassing sites along two neighboring faults in NW Bohemia, central Europe , 2014 .
[16] F. Weinlich. Carbon dioxide controlled earthquake distribution pattern in the NW Bohemian swarm earthquake region, western Eger Rift, Czech Republic – gas migration in the crystalline basement , 2014 .
[17] Tomáš Fischer,et al. Intra-continental earthquake swarms in West-Bohemia and Vogtland: A review , 2014 .
[18] V. Stejskal,et al. Geodynamic processes in the NW Bohemian swarm earthquake region, Czech Republic, identified by continuous gas monitoring , 2013 .
[19] K. Bräuer,et al. CO2 discharge in an active, non-volcanic continental rift area (Czech Republic): Characterisation (δ13C, 3He/4He) and quantification of diffuse and vent CO2 emissions , 2013 .
[20] P. Hrubcová,et al. Moho depth determination from waveforms of microearthquakes in the West Bohemia/Vogtland swarm area , 2013 .
[21] Ute Weckmann,et al. Correlation between deep fluids, tremor and creep along the central San Andreas fault , 2011, Nature.
[22] Jeffrey S. Ovall,et al. A parallel goal-oriented adaptive finite element method for 2.5-D electromagnetic modelling , 2011 .
[23] U. Weckmann,et al. Making and Breaking of a Continent: Following the Scent of Geodynamic Imprints on the African Continent Using Electromagnetics , 2011, Surveys in Geophysics.
[24] Max A. Meju,et al. Crustal deformation of the eastern Tibetan plateau revealed by magnetotelluric imaging , 2010 .
[25] K. Bräuer,et al. Earthquake swarms in non‐volcanic regions: What fluids have to say , 2009 .
[26] A. Brauer,et al. Discovery of the first Quaternary maar in the Bohemian Massif, Central Europe, based on combined geophysical and geological surveys , 2009 .
[27] T. Fischer,et al. Role of crustal fluids in triggering the West Bohemia/Vogtland earthquake swarms: Just what we know (a review) , 2008 .
[28] A. Mateus,et al. Unraveling middle-crust conductive layers in Paleozoic Orogens through 3D modeling of magnetotelluric data : The Ossa-Morena Zone case study (SW Iberian Variscides) , 2008 .
[29] K. Bräuer,et al. Natural laboratory NW Bohemia: Comprehensive fluid studies between 1992 and 2005 used to trace geodynamic processes , 2008 .
[30] Tomáš Fischer,et al. Intraplate seismicity in the western Bohemian Massif (central Europe): A possible correlation with a paleoplate junction , 2007 .
[31] W. Seifert,et al. Petrological and seismic studies of the lithosphere in the earthquake swarm region Vogtland/NW Bohemia, central Europe , 2007 .
[32] H. Kämpf,et al. Seismic evidence for asthenospheric updoming beneath the western Bohemian Massif, central Europe , 2006 .
[33] G. Marquis,et al. Crustal rheology of the Himalaya and Southern Tibet inferred from magnetotelluric data , 2005, Nature.
[34] Ute Weckmann,et al. Effective noise separation for magnetotelluric single site data processing using a frequency domain selection scheme , 2005 .
[35] S. Shapiro,et al. Evidence for triggering of the Vogtland swarms 2000 by pore pressure diffusion , 2005 .
[36] A. Hemmann,et al. Earthquake swarms in the Vogtland/Western Bohemia region: Spatial distribution and magnitude–frequency distribution as an indication of the genesis of swarms? , 2005 .
[37] Yosihiko Ogata,et al. Detecting fluid signals in seismicity data through statistical earthquake modeling , 2005 .
[38] K. Bräuer,et al. Evidence for ascending upper mantle‐derived melt beneath the Cheb basin, central Europe , 2005 .
[39] H. Kümpel,et al. The KTB Deep Crustal Laboratory and the western Eger Graben , 2005 .
[40] Paul A. Bedrosian,et al. Electrical conductivity images of active and fossil fault zones , 2005, Geological Society, London, Special Publications.
[41] M. Becken,et al. An ellipticity criterion in magnetotelluric tensor analysis , 2004 .
[42] K. Bräuer,et al. Isotopic evidence (3He/4He, of fluid‐triggered intraplate seismicity , 2003 .
[43] P. Bankwitz,et al. Structural characteristics of epicentral areas in Central Europe: study case Cheb Basin (Czech Republic) , 2003 .
[44] Yoshimori Honkura,et al. Magnetotelluric imaging of fluids in intraplate earthquake zones, NE Japan Back Arc , 2001 .
[45] William Rodi,et al. Nonlinear conjugate gradients algorithm for 2-D magnetotelluric inversion , 2001 .
[46] Johnston,et al. Dilational processes accompanying earthquakes in the long valley caldera , 2000, Science.
[47] K. Bräuer,et al. An active subcontinental mantle volatile system in the western Eger rift, Central Europe: Gas flux, isotopic (He, C, and N) and compositional fingerprints , 1999 .
[48] Oliver Ritter,et al. New equipment and processing for magnetotelluric remote reference observations , 1998 .
[49] S. Mueller,et al. The European Cenozoic rift system , 1996 .
[50] W. Mooney,et al. Seismic evidence for active magmatic underplating beneath the Basin and Range Province, western United States , 1993 .
[51] K. Vozoff,et al. Magnetotellurics: Principles and practice , 1990, Journal of Earth System Science.
[52] H. Maluski,et al. Terrane boundaries in the Bohemian Massif: Result of large-scale Variscan shearing , 1990 .
[53] W. Franke. Tectonostratigraphic units in the Variscan belt of central Europe , 1989 .
[54] R. Parker. The inverse problem of electromagnetic induction: Existence and construction of solutions based on incomplete data , 1980 .