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THE EFFECTS OF DEPOSITIONAL ENVIRONMENT ON DETRITAL MINERALOGY. THE PERMIAN CUTLER-CEDAR MESA FACIES TRANSITION, NEAR MOAB, UTAH.MACK GH.1977; DISSERT. ABSTR. INTERNATION., B; U.S.A.; DA. 1977; VOL. 38; NO 4; PP. 1618.B-1619.B; RESUMEArticle

DEPOSITIONAL ENVIRONMENTS OF THE CUTLER-CEDAR MESA FACIES TRANSITION (PERMIAN) NEAR MOAB, UTAH.MACK GH.1977; MOUNT. GEOLOGIST; U.S.A.; DA. 1977; VOL. 14; NO 2; PP. 53-68; BIBL. 2 P.; 9 ILL.Article

THE SURVIVABILITY OF LABILE LIGHT-MINERAL GRAINS IN FLUVIAL, AEOLIAN AND LITTORAL MARINE ENVIRONMENTS: THE PERMIAN CUTLER AND CEDAR MESA FORMATIONS, MOAB, UTAHMACK GH.1978; SEDIMENTOLOGY; NLD; DA. 1978; VOL. 25; NO 5; PP. 587-604; BIBL. 2 P.; 9 ILL.Article

EFFECT OF A SHALLOW MARINE ENVIRONMENT ON DETRITAL MINERALOGY, THE PERMIAN CUTLER AND CEDAR MESA SANDSTONES IN SOUTHEAST UTAH.MACK GH.1976; GEOL. SOC. AMER., ABSTR. PROGRAMS; U.S.A.; DA. 1976; VOL. 8; NO 6; PP. 991-992Conference Paper

PENNSYLVANIAN MUD MOUND, HERMOSA GROUP, SOUTHEASTERN COLORADO = MONTICULE DE VASE DU PENNSYLVANIEN, GROUPE HERMOSA, COLORADO DU SUD-ESTMACK GH; MILLER ML.1980; MT. GEOL.; ISSN 0027-254X; USA; DA. 1980; VOL. 17; NO 2; PP. 37-43; BIBL. 20 REF.; ESQUISSE/ILL.Article

PALEOCLIMATE INTERPRETATION FROM A PETROGRAPHIC COMPARISON OF HOLOCENE SANDS AND THE FOUNTAIN FORMATION (PENNSYLVANIAN) IN THE COLORADO FRONT RANGE.MACK GH; SUTTNER LJ.1977; J. SEDIMENT. PETROL.; U.S.A.; DA. 1977; VOL. 47; NO 1; PP. 89-100; BIBL. 28 REF.; 6 ILL.Article

PALEOCLIMATE INTERPRETATION FROM A PETROGRAPHIC COMPARISON OF HOLOCENE SANDS AND THE FOUNTAIN FORMATION (PENNSYLVANIAN) IN THE COLORADO FRONT RANGE: DISCUSSION, REPLYWALKER TR; SUTTNER LJ; MACK GH et al.1978; J. SEDIMENT. PETROL.; USA; DA. 1978; VOL. 48; NO 3; PP. 1011-1016; BIBL. DISSEM.Article

RE-EVALUATION OF THE USE OF UNDULATORY EXTINCTION AND POLYCRYSTALLINITY IN DETRITAL QUARTZ FOR PROVENANCE INTERPRETATION.BASU A; YOUNG SW; SUTTNER LJ et al.1975; J. SEDIMENT. PETROL.; U.S.A.; 1975, VOL. 45, NUM. 0004, P. 873 A 882Serial Issue