OROGENIC VOLCANISM CAUSED BY THERMAL RUNAWAYS. = VOLCANISME OROGENIQUE DU AUX ELEVATIONS THERMIQUES.SPOHN T.1980; GEOPHYS. J.R. ASTR. SOC.; GBR; DA. 1980; VOL. 62; NO 2; PP. 403-419; BIBL. 40 REF.; 2 TAB. ; TABL./ILL.Article

REAKTIONSKINETISCHE UNTERSUCHUNGEN ZUR METAMORPHOSE IN DER KONTINENTALEN UNTERKRUSTE = ETUDES DE CINETIQUE DES REACTIONS DU METAMORPHISME DANS LA CROUTE CONTINENTALE INFERIEURESPOHN T.1979; JTAG. DTSCH. GEOPHYS. GESELLSCH.; DEU; DA. 1979; VOL. 39; PP. 118Conference Paper

UEBER DIE ENTSTEHUNG VON ANDESITISCHEM VULKANISMUS = SUR LA FORMATION DU VOLCANISME ANDESITIQUESPOHN T.1980; BERLIN. GEOWISSENSCH. ABH., REIHE A GEOL. PALAEONTOL.; ISSN 0172-8784; DEU; DA. 1980; VOL. 19; PP. 225Article

Thinning of moving lithosphere plates by mantle plumes = Amincissement des plaques lithosphériques mobiles par des panaches mantelliquesSPOHN, T.International meeting on geothermics and geothermal energy. 1986, 86Conference Paper

LATE STAGE DEVELOPMENT OF MATURE ATLANTIC-TYPE CONTINENTAL MARGINS = DERNIERE ETAPE DE L'ACHEVEMENT DES MARGES CONTINENTALES DE TYPE ATLANTIQUENEUGEBAUER HJ; SPOHN T.1980; OCEANIC RIDGES AND ARCS. GEODYNAMIC PROCESSES; NLD/GBR/USA; AMSTERDAM: ELSEVIER/OXFORD: ELSEVIER/NEW YORK: ELSEVIER; DA. 1980; PP. 279-309; BIBL. 3 P.; 1 TAB. ; ILL./ESQUISSE/TABL.Book Chapter

ZUR ABSENKUNG VON KONTINENTALEN SEDIMENTBECKEN = LA SUBSIDENCE DES BASSINS SEDIMENTAIRES CONTINENTAUXNEUGEBAUER HJ; SPOHN T.1979; JTAG. DTSCH. GEOPHYS. GESELLSCH.; DEU; DA. 1979; VOL. 39; PP. 114Conference Paper

LATE STAGE DEVELOPMENT OF MATURE ATLANTIC-TYPE CONTINENTAL MARGINSNEUGEBAUER HJ; SPOHN T.1978; TECTONOPHYSICS; NLD; DA. 1978; VOL. 50; NO 2-3; PP. 275-305; BIBL. 3 P.Article

METASTABLE PHASE TRANSITION MODELS AND THEIR BEARING ON THE DEVELOPMENT OF ATLANTIC-TYPE GEOSYNCLINESSPOHN T; NEUGEBAUER HJ.1978; TECTONOPHYSICS; NLD; DA. 1978; VOL. 50; NO 2-3; PP. 387-412; BIBL. 2 P.; 16 ILL.Article

VERTIKALBEWEGUNGEN DER ERDKRUSTE = MOUVEMENTS VERTICAUX DE LA CROUTE TERRESTRENEUGEBAUER HJ; SPOHN T; TOBIAS E et al.1975; FORSCHUNGSBER. JOHANN WOLFGANG GOETHE-UNIV., FACHBEREICH GEOWISS.; DEU; DA. 1975; VOL. 2; PP. 96-97; BIBL. 2 REF.Article

Crystallization calculations for a binary melt cooling at constant rates of heat removal : implications for the crystallization of magma bodiesHORT, M; SPOHN, T.Earth and planetary science letters. 1991, Vol 107, Num 3-4, pp 463-474, issn 0012-821XArticle

Thermal equilibration of the Earth following a giant impactSPOHN, T; SCHUBERT, G.Geophysical journal international. 1991, Vol 107, Num 1, pp 163-170Article

Thermal-orbital histories of viscoelastic models of Io (J1) = Histoires thermiques et orbites dans les modèles viscoélastiques de Io (J1)FISCHER, H.-J; SPOHN, T.Icarus (New York, NY). 1990, Vol 83, Num 1, pp 39-65, issn 0019-1035Article

Vertical structure of the head of a cylindrical mantle plume from a model of two-phase flow with meltingLI YINTING; SPOHN, T.Geophysical journal international. 1991, Vol 107, Num 1, pp 103-115Article

Two-dimensional stokes flow around a heated cylinder : A possible application for diapirs in the mantleZIETHE, R; SPOHN, T.Journal of geophysical research. 2007, Vol 112, Num B9, issn 0148-0227, B09403.1-B09403.13Article

Differentiation and thermal history of Mars : Implications for the topographical stability of Martian volcanismSPOHN, T; BREUER, D.International geological congress. 1992, p.652Conference Paper

Early plate tectonics versus single-plate tectonics on Mars: Evidence from magnetic field history and crust evolutionBREUER, D; SPOHN, T.Journal of geophysical research. 2003, Vol 108, Num E7, pp 8.1-8.13, issn 0148-0227Article

Possible flush instability in mantle convection at the Archaean-Proterozoic transitionBREUER, D; SPOHN, T.Nature (London). 1995, Vol 378, Num 6557, pp 608-610, issn 0028-0836Article

Continental growth and recycling and the thermal evolution of the EarthBREUER, D; SPOHN, T.International geological congress. 1992, 2Vol, p. 46Conference Paper

Differentiation and core formation in accreting planetesimalsNEUMANN, W; BREUER, D; SPOHN, T et al.Astronomy and astrophysics (Berlin. Print). 2012, Vol 543, issn 0004-6361, A141.1-A141.21, 2Article

Mantle differentiation and the crustal dichotomy of MarsBREUER, D; SPOHN, T; WÜLLNER, U et al.Planetary and space science. 1993, Vol 41, Num 4, pp 269-283, issn 0032-0633Article

A model for the interior structure, evolution, and differentiation of CallistoNAGEL, K; BREUER, D; SPOHN, T et al.Icarus (New York, NY). 2004, Vol 169, Num 2, pp 402-412, issn 0019-1035, 11 p.Article

The interior structure of Mars : Implications from SNC meteoritesSOHL, F; SPOHN, T.Journal of geophysical research. 1997, Vol 102, Num E1, pp 1613-1635, issn 0148-0227Conference Paper

Symmetries of volcanic distributions on Mars and Earth and their mantle plume dynamicsMATYSKA, C; YUEN, D. A; BREUER, D et al.Journal of geophysical research. 1998, Vol 103, Num E12, pp 28587-28597, issn 0148-0227Article

Thermal model of the MUPUS penetratorSEWERYN, K; BANASZKIEWICZ, M; GRUNWALD, M et al.International journal of heat and mass transfer. 2005, Vol 48, Num 18, pp 3713-3721, issn 0017-9310, 9 p.Article

Three dimensional models of Martian mantle convection with phase transitionsBREUER, D; YUEN, D. A; SPOHN, T et al.Geophysical research letters. 1998, Vol 25, Num 3, pp 229-232, issn 0094-8276Article