au.\*:("FORSYTH DW")
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COMPARISON OF MECHANICAL MODELS OF THE OCEANIC LITHOSPHERE = COMPARAISON DES MODELES MECANIQUES DE LITHOSPHERE OCEANIQUEFORSYTH DW.1980; J. GEOPHYS. RES.; ISSN 0022-1406; USA; DA. 1980; VOL. 85; NO 11; PP. 6364-6368; BIBL. 30 REF.Article
THE EVOLUTION OF THE UPPER MANTLE BENEATH MID-OCEAN RIDGES.FORSYTH DW.1977; TECTONOPHYSICS; NETHERL.; DA. 1977; VOL. 38; NO 1-2; PP. 89-118; BIBL. 4 P.; 12 ILL.Article
THE EARLY STRUCTURAL EVOLUTION AND ANISOTROPY OF THE OCEANIC UPPER MANTLE.FORSYTH DW.1975; GEOPHYS. J. R ASTR. SOC.; G.B.; DA. 1975; VOL. 43; NO 1; PP. 103-162; BIBL. 4 P. 1/2Article
CRUSTAL STRUCTURE AND ISOSTATIC COMPENSATION NEAR THE KANE FRACTURE ZONE FROM TOPOGRAPHY AND GRAVITY MEASUREMENTS. I: SPECTRAL ANALYSIS APPROACH = STRUCTURE CRUSTALE ET COMPENSATION ISOSTATIQUE PRES DE LA ZONE DE FRACTURE KANE D'APRES LES MESURES TOPOGRAPHIQUES ET GRAVIMETRIQUES. I: APPROCHE D'ANALYSE SPECTRALELOUDEN KE; FORSYTH DW.1982; GEOPHYS. J.R. ASTRON. SOC.; ISSN 0016-8009; GBR; DA. 1982; VOL. 68; NO 3; PP. 725-750; BIBL. 2 P.; ILL.Article
A DETAILED STUDY OF TWO EARTHQUAKES SEAWARD OF THE TONGA TRENCH. IMPLICATIONS FOR MECHANICAL BEHAVIOR OF THE OCEANIC LITHOSPHERECHEN T; FORSYTH DW.1978; J. GEOPHYS. RES.; USA; DA. 1978; VOL. 83; NO 10; PP. 4995-5003; BIBL. 36 REF.Article
THE OCCURRENCE OF ANOMALOUS SEISMIC EVENTS IN EASTERN TIBET.TATHAM RH; FORSYTH DW; SYKES LR et al.1976; GEOPHYS. J. R. ASTR. SOC.; G.B.; DA. 1976; VOL. 45; NO 3; PP. 451-481; BIBL. 2 P.Article
THE OCCURRENCE OF ANOMALOUS SEISMIC EVENTS IN EASTERN TIBET.TATHAM RH; FORSYTH DW; SYKES LR et al.1976; GEOPHYS. J. R. ASTR. SOC.; G.B.; DA. 1976; VOL. 45; NO 3; PP. 451-481; BIBL. 55 REF.; 14 ILL.Article
FAULT PLANE SOLUTIONS OF EARTHQUAKES ON THE NAZCA PLATE BOUNDARIES AND THE EASTER PLATE1,2.ANDERSON RN; FORSYTH DW; MOLNAR P et al.1974; EARTH PLANET. SCI. LETTERS; NETHERL.; DA. 1974; VOL. 24; NO 2; PP. 188-202; BIBL. 36 REF.; 7 ILL.Article