List of publications, H. Schmeling

 

In press

Shahraki, M. and H. Schmeling, 2012: Plume-induced geoid anomalies from 2D axi-symmetric temperature- and pressure dependent mantle convection models.  J. Geodynamics., in press.

Richard, G. C., S. Kanjilal, H. Schmeling, 2012: Solitary-waves in geophysical two-phase viscous media : a semi-analytical solution. Phys. Earth Planet. Int., in presss

 

2012

Burchardt, S., H Koyi, H. Schmeling, L Fuchs, 2012 Sinking of anhydrite blocks within a salt diapir: modeling the influence of block orientation and salt stratification. Geophys. J. Int., DOI: 10.1111/j.1365-246X.2011.05290.x

Burchardt, S., H. Koyi, and H. Schmeling, 2012:The influence of viscosity contrasts on the 1 strain pattern and magnitude within and around dense blocks sinking through Newtonian salt. J. Struct. Geol., 35, 102 – 116

Crameri, F., H. Schmeling, G. J. Golabek, T. Duretz, R. Orendt, S.J.H. Buiter, D. A. May, B. J. P. Kaus, T. V. Gerya and P. J. Tackley, 2012. A comparison of numerical surface topography calculations in geodynamic modelling: An evaluation of the `sticky air' method. Geophys. J. Int., 189, 38 -54,doi: 10.1111/j.1365-246X.2012.05388.x

 

2011

Fuchs, L., Schmeling, H., and H. Koyi, 2011: Numerical models of salt diapir formation by down-building: the role of sedimentation rate, viscosity contrast, initial amplitude, and wavelength. Geophys. J. Int., 186, 390 – 400.  doi: 10.1111/j.1365-246X.2011.05058.x

Wallner, H. and H. Schmeling, 2011: Sensitivity Analysis of Rift Induced Delamination with Application to Rwenzori Mountains. Geophys. J. Int., doi: 10.1111/j.1365-246X.2011.05237.x

Burchardt, S., H. Koyi and H. Schmeling, 2011: Strain pattern within and around denser blocks sinking within Newtonian salt structures. J. Struct. Geol., 33, 145 – 153

 

2010

Schmeling, H., 2010: Crustal accretion at anomalous spreading centres: Rheological control of crustal thickness. Phys. Earth Planet. Int, 183, 447 – 455.

Wallner, H. and H. Schmeling, 2010: Rift induced delamination of mantle lithosphere and crustal uplift: A new mechanism for explaining Rwenzori Mountain’s extreme elevation? International Journal of Earth Sciences, online first, doi 10.1007/s00531-010-0521-6

 

2009

Schmeling, H., 2009: Dynamic models of continental rifting with melt generation. Tectonophysics,Volume 480, Issues 1-4, 5 January 2010, Pages 33-47

Bjarnason, I. T. and H. Schmeling, 2009: The structure of the lithosphere and asthenosphere of Iceland from surface waves. Geophys. J. Int. , 178, 394 – 418.. doi: 10.1111/j.1365-246X.2009.04155.x

Tetzlaff, M. and H. Schmeling, 2009: Time-dependent interaction between subduction dynamics and phase transition kinetics. Geophys. J. Int., 178, 826 – 844. doi: 10.1111/j.1365-246X.2009.04182.x

Chemia, Z., H. Schmeling, H. Koyi, 2009:  The effect of the salt viscosity on future evolution of the Gorleben salt diapir, Germany. Tectonophysics, 473, 446 – 456.

 

2008

Schmeling, H., A.Y. Babeyko, A. Enns, C. Faccenna, F. Funiciello, T. Gerya, G.J. Golabek, S. Grigull, B.J.P. Kaus, G. Morra, S. Schmalholz, J. van Hunen, 2008: A benchmark comparison of spontaneous subduction models – towards a free surface, Phys. Earth. Planet. Int., 171, 198 – 223, Reprint available see below*, preprint

Ruedas, T. and H.Schmeling, 2008: Kinematic models for the thickness of oceanic crust at and near mid-oceanic spreading centers. J. Geophys. Res., 113,B01402, doi:10.1029/2006JB004746. Reprint available, see below *

Ruedas, T., H.Schmeling, 2008: On the orientation of tensile dikes in a ridge-centered plume. Tectonophysics, 447, 19 - 30. doi:10.1016/j.tecto.2006.01.030. Reprint available, see below *

Schmeling, H., Marquart, G., 2008: Crustal accretion and dynamic feedback on mantle melting of a ridge centred plume: the Iceland case. Tectonophysics.. 447, 31 – 52. doi:10.1016/j.tecto.2006.08.012. Reprint available, see below *

Mihalffy, P., B. Steinberger, and H. Schmeling, 2008: The effect of the large-scale mantle flow field on the Iceland hotspot track. Tectonophysics, 447, 5 - 18. doi:10.1016/j.tecto.2006.12.012.

Golabek, G. J, H. Schmeling, and P. J. Tackley, 2008: Earth's core formation aided by flow channelling instabilities induced by iron diapirs, Earth Planet. Sci. Lett., 271, 24-33. doi:10.1016/j.epsl.2008.02.033. Preprint available, see below *

 

2007

Ruedas, T., Marquart, G. and H. Schmeling, 2007: Iceland : The current picture of a ridge-centred mantle plume. In: Mantleplumes – a multidisciplinary approach. Eds J. Ritter and U. R. Christensen.p.71 - 126, Springer,  ISBN: 978-3-540-68045-1

Marquart, G., H. Schmeling, O. Cadek, 2007: Dynamic models for flow and seismic anisotropy in the North Atlantic and comparison with observations, Geochem. Geophys. Geosyst., 8,Q02008, doi:10.1029/2006GC001359. Reprint available, see below *

 

2006

Schmeling, H., 2006: A model of episodic melt extraction for plumes. J. Geophys. Res., 111, B03202, doi:10.1029/2004JB003423. Reprint available, see below *

 

2005

Enns, A. , Th. W. Becker, and H. Schmeling, 2005: The dynamics of subduction and trench migration for viscositystratification Geophys. J. Int., 160, 761–775, Preprint

Maumus, J., N. Bagdassarov, H. Schmeling, 2005: Electrical conductivity and partial melting of mafic rocks under pressure. Geochim. Cosmochim. Acta, 69(19), 4703 – 4718.

 

2004

Marquart, G. and H. Schmeling, 2004: A Dynamic Model for the Iceland Plume and the North Atlantic based on Tomography and Gravity Data, Geophy. J. Int., 159, 40 - 52, Reprint available, see below*

Ilk, K.H., J. Flury, R. Rummel, P. Schwintzer,W. Bosch, C. Haas, J. Schröter, D. Stammer, W. Zahel, H. Miller, R. Dietrich,P. Huybrechts, H. Schmeling, D. Wolf, J. Riegger, A. Bardossy, A. Güntner,2004: Mass Transport and Mass Distribution in the Earth System - Contributionof the New Generation of Satellite Gravity and Altimetry Missions to Geosciences, Proposal for a German Priority Research Program, pdf-version (52 Mbyte!)

Ruedas, T., H. Schmeling, G. Marquart, A.Kreutmann, A. Junge, 2004: Temperature and melting of a ridge-centered plumewith application to Iceland, part I: Dynamics and crust production. Geophys. J.Int., 158(2),729-743.743  Reprint available, see below *

Kreutzmann, A.,H. Schmeling, A. Junge, T. Ruedas, G. Marquart, I. Th. Bjarnason, 2004: Temperature and  meltingof a ridge-centered plume with application to Iceland, part II: Predictions for electromagnetic and seismic observables. Geophys. J. Int.,  159, 1097 -1111 Reprintavailable, see below *

 

2003

Schmeling, H., G. Marquart, T. Ruedas, 2003:Pressure- and temperature-dependent thermal expansivity and the effect onmantle convection and surface observables. Geophys. J. Int., 154, 224–229. Reprint available, see below *

Müller, K., N. Bagdassarov, H. Schmeling, 2003:Internal friction spectroscopy in Li2O-2-SiO2 partially crystallised glasses. J. Non-Crystalline Solids, 319, 44 - 56.

Bagdassarov N.,Maumus J., Schmeling H., 2003: Elektrische Eigenschaften teilgeschmolzener  Gesteine an der mittelozeanischen Spreizungsachse, Mitteilungen der Deutschen Gesellschaft  für Meeresforschung, Heft 2-3/2003, pdf-file

 

1980 - 2002

Schmeling, H., A.Junge, G. Marquart, T. Ruedas, A. Kreutzmann, 2002: Island, Vulkaninsel auf dem Mittelatlantischen Rücken: Erkundung der tiefen Ursachen durch geophysikalische Modellierungen. Kleine Senckenberg-Reihe 43, A. Junge (Hrsg.), 161 - 170, pdf-file

Steinberger, B., H. Schmeling and G. Marquart,2001: Large-scale lithospheric stress field   and topography induced by global mantle circulation. Earth Planet. Sci. Lett., 186, 75-91.

Arnold, J., W. R. Jacoby, H. Schmeling, B.Schott, 2001: Continental collision and the  dynamic and thermal evolution of the Variscan orogeniccrustal root - numerical models.  J.Geodynamics, 31, 273 - 291.

Schott, B., D. A. Yuen, and H. Schmeling, 2000:The significance of shear heating in continental convergent processes. Phys. Earth Planet. Int., 118(3-4), pp. 273--290.

Schott, B., D. A.Yuen, and H. Schmeling, 2000:The diversity of tectonics from fluid-dynamical modeling of the lithosphere-mantle system. Tectonophysics, 322, 35 - 51.

Schmeling, H., 2000: Partial melting and melt segregation in a convecting mantle. In: Physics and Chemistry of PartiallyMolten Rocks, eds. N. Bagdassarov, D. Laporte,  and A.B. Thompson, Kluwer Academic Publ., Dordrecht, pp. 141- 178. pdf for download

Marquart, G., H. Schmeling, G. Ito, B. Schott,2000: Conditions for plumes to penetrate the mantle phase boundaries. J.Geophys. Res., 105, 5679-5693.

Tetzlaff, M. and H. Schmeling, 2000: The influence of olivine metastability on deep subduction of oceanic lithosphere. Phys. Earth Planet. Int.120, 29-38.

Marquart, G. , H. Schmeling, 2000: Interactionof Mantel Plumes with the Spinell-Perovskite Phase Boundary: Implications for Chemical Mixing, Earth and Planet. Sci. Lett., 177,  241 - 254

Koyi, H. A., A. G. Milnes, H. Schmeling, C. J.Talbot and H. Zeyen, 1999: Numerical models of ductile rebound of crustal roots beneath mountain belts. Geophys. J. Int.,  139, 556 - 562.

Marquart, G., H.Schmeling & A. Braun, 1999. Small Scale Instabilities below the cooling oceanic lithosphere, Geophys. J. Int.,138, 655 - 666.

Schmeling, H., R. Monz, and D. C. Rubie, 1999: The influence of olivine metastability on the dynamics of subduction., Earth Planet. Sci. Lett.., 165,55 - 66.

Schott, B., D.A. Yuen and H. Schmeling, 1999: Viscous heating in heterogeneousmedia as applied to thermal interaction between the crust and mantle. GRL,26,513-516.

Schott, B. and H. Schmeling, 1998: Delamination and detachment of a lithospheric root. Tectonophysics, 296, 225 - 247.

Becker, T. W. and H. Schmeling, 1998: Earthquake recurrence time variations with and without fault zone interactions. Geophys.J. Int., 135, 165 - 176

Simakin, A., H. Schmeling, and V. Trubitsyn,1997: Purely sedimentative convection with constant crystal flux from above.Phys. Earth Planet. Int., 102, 185-200.

van Keken, P., S. King, H. Schmeling, U.Christensen, D. Neumeister, M.-P. Doin, 1997:  A comparison of methods for the modeling of thermochemical convection. J. Geophys.  Res., 102, 22477 - 22495. .

Schmeling, H. and G. Y. Bussod, 1996: Variable viscosity convection and partial melting in the continental asthenosphere. J.Geophys. Res., 101, 5411 - 5423. Reprint available, see below *

Bittner, D. and H. Schmeling, 1995: Numerical modelling of melting processes and induced diapirism in the lower crust. Geophys. J. Int., 123, 59-70.

Cruden, A. R., H. Koyi, and H. Schmeling, 1995:Diapiric basal entrainment of mafic into felsic magma. Earth Planet. Sci.Lett., 131,. 321 - 340.

Simakin, A., V. Trubitsyn, and H. Schmeling,1994: Structure of the upper boundary layer of a solidifying intrusion with crystal sedimentation. Earth Planet. Sci. Lett., 126, 333-349.

Schmeling, H. and G. Marquart, 1993: Mantle flow and the evolution of the lithosphere. Phys. Earth Planet. Int., 79, 241-267.

Weinberg, R. F., and H. Schmeling,1992: Polydiapirs: Multiwave length gravity structures.  J. Struct.Geol., 14, 425-436..

Schmeling, H., 1991: Variable viscosity convection in a compressible upper mantle and the thickness of continental lithosphere. in: Glacial Isostacy, Sea-Level and Mantle Rheology, ed.: R.Sabadini, K. Lambeck, E. Boschi, Kluwer Academic Publishers,  Dordrecht, P. 607-636.

Talbot, C. J., Rönnlund, P., Schmeling, H.,Koyi,H., and Jackson, M. A., 1991: Diapiric spoke patterns. Tectonophysics,188, 187-201.

Schmeling, H. and G. Marquart, 1991: The influence of second scale convection on the thickness of the continental lithosphere and crust. Tectonophysics. 189, 281-306.

Schmeling, H., and G. Marquart, 1990: A mechanism for crustal thinning without lateral extension. Geophys. Res. Lett.,17, 2417-2420.

Schmeling, H., 1989b: Compressible convection with constant and variable viscosity: the effect on geoid, topography, and slab formation, J. Geophys. Res., 94, 12463-12481.  pdf-reprint

Marquart, G. and Schmeling, H., 1989: Topography and geoid undulations caused by small scale convection beneath continental lithosphere of variable elastic thickness. J. Geophys., 97,511-527. pdf

Schmeling, H., 1988: Numerical models of Rayleigh-Taylor instabilities superimposed upon convection. Bulletin of the Geological Institutions of the University of Uppsala, 14. pp. 95 – 109, Uppsala ISSN 0302-2749 Reprint

Schmeling, H., Cruden, A. R., and Marquart, G.,1988: Progressive deformation in and around a fluid sphere moving through aviscous medium: implications for diapiric ascent. Tectonophysics, 149, 17-34.

Blanckenbach, B., Busse, F., Christensen, U.,Cserepes, L. Gunkel, D., Hansen, U., Harder, H. Jarvis, G., Koch, M., Marquart, G., Moore D., Olson, P., and Schmeling, H., 1988: A benchmark comparison for mantle convection codes, J. Geophys., 98, 23-38.     

Schmeling, H., 1987a: On the relation between initial conditions and late stages of Rayleigh- Taylor instabilities. Tectonophysics, 133, 65-80.

Schmeling, H. 1987b: On the interaction between small- and large scale convection and post glacial rebound flow in a power- law mantle. Earth Planet. Sci. Lett., 84, 254-262. Reprint available, see below *

Schmeling, H., 1986a: Numerical models on the influence of partial melt on elastic, anelastic, and electric properties of rocks. Part II: electrical conductivity. Phys. Earth Planet. Int., 43, 123-136.

Schmeling, H., 1986b: A simple statistical model on the degree of interconnection in partially molten rocks. J. Geophys.,59, 142-145.

Weijermars, R. and Schmeling, H., 1986: Scaling of Newtonian and non-Newtonian fluid dynamics without inertia for quantitative modelling of rock flow due to gravity (including the concept of rheological similarity). Phys. Earth Planet. Int., 43, 316-330.

Schmeling, H., 1985a: Partial melt below Iceland: A combined interpretation of seismic and conductivity data. J.Geophys. Res., 90, 10105-10116.

Schmeling, H., 1985b: Numerical models on the influence of partial melt on elastic, anelastic, and electric properties of rocks. Part I: elasticity and anelasticity. Phys. Earth Planet. Int., 41, 34-57. A matlab code can be downloaded here

Schmeling, H., 1983: Numerische Modelle über den Einfluß partieller Schmelze auf elastische, anelastische und elektrische Eigenschaften von Gesteinen mit Anwendung auf Labordaten und die Asthenosphäre (Numerical models on the  influence of partial melt on elastic, anelastic, and electric properties of  rocks with application to laboratory data and the asthenosphere), Dissertation, University Frankfurt/M.

Jacoby, W. R. and Schmeling, H., 1982: On the effects of the lithosphere on mantle convection and evolution. Phys. Earth Planet. Int., 29, 305-319.

 Berckhemer, H., Kampfmann, W., Aulbach, E., and Schmeling, H., 1982: Shear modulus and Q of forsterite and dunite near partial melting from forced-oscillation experiments. Phys. Earth Planet. Int., 29, 30-41.

Schmeling, H. and Jacoby, W. R., 1981: On modelling the lithosphere in mantle convection with non-linear rheology. J. Geophys., 50, 89-100.

Jacoby, W. R. and Schmeling, H., 1981:Convection experiments and the driving mechanism. Geol. Rundschau, 70, 207-230.

Schmeling, H., 1980:Numerische Konvektionsrechnungen unter Annahme verschiedener Viskositätsverteilungen und Rheologien im Mantel (Numerical calculationson  convection assuming various viscosity distributions and rheologies in the mantle). Master thesis (Diplomarbeit). Report of the Institut für Meteorologie und Geophysik, Universität Frankfurt/M, Nr. 4

 

* Reprints are available on request (schmeling@geophysik.uni-frankfurt.de), see also at
http://www.geophysik.uni-frankfurt.de/~schmelin/reprints/


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