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COMPARISON OF SLOPE AND BASINAL SEDIMENTS OF A MARGINAL CRATONIC BASIN (PEDREGOSA BASIN, NEW MEXICO) AND A MARGINAL GEOSYNCLINAL BASIN (SOUTHERN BORDER OF PIEMONTAIS GEOSYNCLINE, BERNINA NAPPE, SWITZERLAND).SCHUPBACH MA.1974; DISSERT. ABSTR. INTERNATION., B; USA; RESUME,1974, VOL. 35, NUM. 0004, P. 1746Serial Issue

TEXTONIK IM GEBIETE DES BERNINAPASSES UND DER VAL CHAMUERA (ENGADIN). = TECTONIQUE DANS LA REGION DU COL DE BERNINA ET DU VAL CHAMUERA ENGADINE)SCHUPBACH MA.1976; ECLOGAE GEOL. HELV.; SUISSE; DA. 1976; VOL. 69; NO 1; PP. 63-73; ABS. ANGL.; BIBL. 20 REF.; 5 ILL.Article

FANS AND CHANNELS IN CLASSICAL FLYSCH, CENTRAL ALPS.SCHUPBACH MA; MOREL R.1974; IN: ANNU. MEET. AM. ASSOC. PET. GEOL. SOC. ECON. PALEONTOL. MINERAL.; SAN ANTONIO, TEX.; 1974; TULSA AM. ASSOC. PET. GEOL.; RESUME,1974, VOL. 1, P. 80 A 81Miscellaneous

STRUCTURAL FRAMEWORK AND DEPOSITIONAL HISTORY OF THE HIGH ATLAS MOUNTAINS, MOROCCO.WARME JE; SCHUPBACH MA; EVANS I et al.1974; IN: ANNU. MEET. AM. ASSOC. PET. GEOL. SOC. ECON. PALEONTOL. MINERAL.; SAN ANTONIO, TEX.; 1974; TULSA AM. ASSOC. PET. GEOL.; RESUME,1974, VOL. 1, P. 95Miscellaneous

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