GEOPHYSICAL INVESTIGATIONS OF DUFEK INTRUSION, PENSACOLA MOUNTAINS, 1978-79 = ETUDES GEOPHYSIQUES DE L'INTRUSION DUFEK, MONTS PENSACOLA, 1978-79ENGLAND AW; COOKE JE; HODGE SM et al.1979; ANTARCT. J.U.S.; ISSN 0003-5335; USA; DA. 1979; VOL. 14; NO 5; PP. 4-5; BIBL. 6 REF.Article

DENSITY OF THE STRATIFORM DUFEK INTRUSION, PENSACOLA MOUNTAIN, ANTARCTICAFORD AB; NELSON SW.1972; ANTARCT. J. U.S.; U.S.A. ; 1972, VOL. 7, NUM. 0005, P. 147 A 149Serial Issue

K/Ar-Altersdatierungen an Magmatiten der Pensacola Mountains (Antarktika) = Datation K/Ar de magmatites des monts Pensacola (Antarctique)KAISER, G; KLEMM, W; WEBER, W et al.Zeitschrift für geologische Wissenschaften. 1982, Vol 10, Num 4, pp 527-530, issn 0303-4534Article

POTASSIUM-ARGON AGES OF DUFEK INTRUSION AND OTHER MESOZOIC MAFIC BODIES IN THE PENSACOLA MOUNTAINS = DATATION AU POTASSIUM-ARGON DE L'INTRUSION DUFEK ET D'AUTRES CORPS MAFIQUES DU MESOZOIQUE DANS LES MONTS PENSACOLAKISTLER RW; FORD AB.1979; ANTARCT. J.U.S.; ISSN 0003-5335; USA; DA. 1979; VOL. 14; NO 5; PP. 8-9; BIBL. 7 REF.Article

PETROLOGIC STUDIES OF THE DUFEK INTRUSION, PENSACOLA MOUNTAINS: IRON-TITANIUM OXIDES.HIMMELBERG GR; FORD AB.1975; ANTARCT. J. U.S.; U.S.A.; DA. 1975; VOL. 10; NO 5; PP. 241-244; BIBL. 10 REF.; 2 ILL.Article

Reconnaissance of minor metal abundances and possible resources of the Dufek intrusion, Pensacola mountains = Reconnaissance des abondances en métaux mineurs et ressources possibles de l'intrusion Dufek, Monts Pensacola, AntarctiqueFORD, A. B; MAYS, R. E; HAFFTY, J et al.Antarctic earth science. International symposium. 4. 1983, pp 433-436Conference Paper

ZUM STRUKTURGEOLOGISCHEN BAU AM WESTRAND DER OSTANTARKTISCHEN TAFEL = LA STRUCTURE GEOLOGIQUE DU BORD OUEST DE LA PLATEFORME DE L'ANTARCTIQUE ESTHOFMANN J; PAECH HJ.1980; Z. GEOL. WISS.; ISSN 0303-4534; DDR; DA. 1980; VOL. 8; NO 4; PP. 425-437; ABS. RUS/ENG; BIBL. 2 P.; 1 TAB. ; ESQUISSE GEOL./TABL./COUPE GEOL.Article

THE GALE MUDSTONE: A PERMIAN (.) TILLITE IN THE PENSACOLA MOUNTAINS AND NEIGHBOURING PARTS OF THE TRANSANTARCTIC MOUNTAINS = LA PELITE GALE: UNE TILLITE DU PERMIEN (.) DANS LES MONTS PENSACOLA ET LES REGIONS VOISINES DES MONTS TRANSANTARCTIQUESNELSON WH.1981; EARTH'S PRE-PLEISTOCENE GLACIAL RECORD; GBR; CAMBRIDGE: CAMBRIDGE UNIV.; DA. 1981; PP. 227-229; BIBL. 13 REF.; ESQUISSEBook Chapter

SOILS FROM THE PENSACOLA MOUNTAINS, ANTARCTICA: PHYSICAL, CHEMICAL AND BIOLOGICAL CHARACTERISTICS = LES SOLS DES MONTS PENSACOLA, ANTARCTIQUE: CARACTERISTIQUES PHYSIQUES, CHIMIQUES ET BIOLOGIQUESPARKER BC; BOYER S; ALLNUTT FCT et al.1982; SOIL BIOL. BIOCHEM.; ISSN 0038-0717; GBR; DA. 1982; VOL. 14; NO 3; PP. 265-271; BIBL. 31 REF.; 5 TAB. ; TABL./ESQUISSE/ILL.Article

K-AR AGE, COMPOSITION, AND ORIGIN OF MESOZOIC MAFIC ROCKS RELATED TO FERRAR GROUP, PENSACOLA MOUNTAINS, ANTARCTICA = AGE AU K-AR, COMPOSITION ET ORIGINE DES ROCHES MAFIQUES MESOZOIQUES RATTACHEES AU GROUPE FERRAR, MONTS PENSACOLA, ANTARCTIQUEFORD AB; KISTLER RW.1980; N.Z. J. GEOL. GEOPHYS.; ISSN 0028-8306; NZL; DA. 1980; VOL. 23; NO 3; PP. 371-390; BIBL. 3 P.Article

The structural development of selected areas in the Pensacola Mountains = Le développement structural de régions particulières dans les Monts Pensacola AntarctiqueFRISCHBUTTER, A; WEBER, W; HOFMANN, J et al.Antarctic earth science. International symposium. 4. 1983, 175Conference Paper

When did open-marine conditions last prevail in the Wilkes and Pensacola Basins, East Antarctica, and when was the Sirus Formation emplaced? = Quand les conditions de mer ouverte ont-elles dominé dans les Bassins Wilkes et Pensacola, Antarctique Est, et quand la Formation Sirius a-t-elle été mise en place?MERCER, J. H.South African journal of science. 1985, Vol 81, Num 5, pp 243-245, issn 0038-2353Conference Paper

Geology and crystallization of the Dufek intrusionFORD, A.B; HIMMELBERG, G.R.The geology of Antarctica. 1991, pp 175-214Book Chapter

Radar-detected englacial stratigraphy in the Pensacola Mountains, Antarctica: implications for recent changes in ice flow and accumulationCAMPBELL, Seth; BALCO, Greg; TODD, Claire et al.Annals of glaciology. 2013, Vol 54, Num 63, pp 91-100, issn 0260-3055, 10 p., 1Article

Latest Neoproterozoic to mid-Cambrian age for the main deformation phases of the Transantarctic Mountains: new stratigraphic and isotopic constraints from the Pensacola Mountains, AntarcticaROWELL, A. J; VAN SCHMUS, W. R; STOREY, B. C et al.Journal of the Geological Society (London). 2001, Vol 158, pp 295-308, issn 0016-7649, 2Article

Early Palaeozoic near-surface deformation in the Neptune Range, Antarctica: implications for the Ross and Gondwanian orogeniesCURTIS, M. L; STOREY, B. C.Journal of the Geological Society (London). 2003, Vol 160, pp 629-642, issn 0016-7649, 14 p., 4Article