DETERMINATION OF REPOSE-PERIOD PATTERNS OF VOLCANOES FROM SEQUENCES OF ASH LAYERS.WICKMAN FE.1970; J. INTERNATION. ASS. MATH. GEOL.; USA; 1970, VOL. 2, NUM. 0003, P. 277 A 283Miscellaneous

METEORITES : SAMPLES OF THE PLANETARY SYSTEM AT LARGE.WICKMAN FE.1969; EARTH MINER. SCI.; USA; 1969(11), VOL. 39, NUM. 0002, P. 9 A 13Miscellaneous

THE IMPACT CENTER OF THE SILJAN STRUCTURE, CENTRAL SWEDEN = CENTRE D'IMPACT DE LA STRUCTURE SILJAN, CENTRE DE LA SUEDEWICKMAN FE.1980; GEOL. FOEREN. STOCKH. FOERH.; ISSN 0016-786X; SWE; DA. 1980; VOL. 102; NO 2; PP. 105-109; BIBL. 3 REF.Article

THE PERCENTAGE BY AREA OF GEOLOGICAL DEPOSITS IN WESTERN CENTRAL SWEDEN AND SOME RELATED PROBLEMSWICKMAN FE.1973; GEOL. FOEREN. STOCKHOLM FOERH.; SWERIGE ; 1973, VOL. 95, NUM. 0553, P. 276 A 280Serial Issue

THE MUONIOANALUSTA METEORITES, WHEN AND WHERE DID THEY FALL.WICKMAN FE.1970; GEOL. FOEREN. STOCKOLM, FOERH.; 1970, VOL. 92, NUM. 0542-03 , P. 404 A 405Miscellaneous

HOW TO EXPRESS TIME IN GEOLOGY.WICKMAN FE.1968; AMER. J. SCI.; USA; 1968(4), VOL. 266, NUM. 0004, P. 316 A 318Miscellaneous

THE CONCEPT OF DOMAIN AND REGIONAL GEOCHEMICAL ABUNDANCES.WICKMAN FE.1969; PROBLEMS.OF.GEOCHEMISTRY-EDITOR.KHITAROV.N.I.; 1969, P. 721 A 726Miscellaneous

DISPLACEMENTS AND THE SILJAN RING STRUCTURE = DEPLACEMENTS DE LA STRUCTURE ANNULAIRE DE SILJANWICKMAN FE.1981; GEOGR. ANN., SER. A; ISSN 0435-3676; SWE; DA. 1981; VOL. 63; NO 3-4; PP. 313-317; BIBL. 11 REF.; ESQUISSE GEOL.Article

ORDER AND RANDOMNESS IN GEOLOGICAL PROCESSES = ORDRE ET HASARD DANS LES PROCESSUS GEOLOGIQUESWICKMAN FE.1981; FUTURE TRENDS IN GEOMATHEMATICS; GBR; LONDON: PION; DA. 1981; PP. 275-280; BIBL. 1 REF.Book Chapter

SWEDISH FIELD-GEOLOGY AT THE CROSS-ROADS: SCIENCE OR SUPERSTITION. = GEOLOGIE DE TERRAIN SUEDOISE AU CROISEMENT: SCIENCE ET SUPERSTITIONWICKMAN FE.1981; GEOL. FOEREN. STOCKH. FOERH.; ISSN 0016-786X; SWE; DA. 1981; VOL. 103; NO 1; PP. 120Conference Paper

MARKOV MODELS OF REPOSE-PERIOD PATTERNS OF VOLCANOES.WICKMAN FE.1976; IN: RANDOM PROCESS GEOL. TWO SYMP.; MONTREAL; 1972; BERLIN SPRINGER; 1976, P. 135 A 161Miscellaneous

REPOSE PERIOD PATTERNS OF VOLCANOES-5-GENERAL DISCUSSION AND A TENTATIVE STOCHASTIC MODEL.WICKMAN FE.1968; ARK. MINERAL. GEOL.; SWE; 1968, VOL. 4, NUM. 0005, P. 351 A 367Miscellaneous

SHOCK EFFECTS IN PEGMATITIC QUARTZ FROM THE SILJAN RING STRUCTURE, CENTRAL SWEDEN = EFFET DE CHOC DANS LE QUARTZ PEGMATITIQUE DE LA STRUCTURE ANNULAIRE DE SILJAN, CENTRE DE LA SUEDETAMMINEN J; WICKMAN FE.1980; GEOL. FOEREN. STOCKH. FOERH.; ISSN 0016-786X; SWE; DA. 1980; VOL. 102; NO 3; PP. 275-278; BIBL. 14 REF.Article

MOLYBDENITE POLYTYPES IN THEORY AND OCCURRENCE. 1. THEORETICAL CONSIDERATIONS OF POLYTYPISM IN MOLYBDENITE.WICKMAN FE; SMITH DK.1970; AMER. MINERALOGIST; USA; 1970, VOL. 55, NUM. 1112, P. 1843 A 1856Miscellaneous

MIDDLE ORDOVICIAN CHONDRITE IN FOSSILIFEROUS LIMESTONE FROM BRUNFLO, CENTRAL SWEDEN = CHONDRITE DE L'ORDOVICIEN MOYEN DANS LES CALCAIRES FOSSILIFERES DE BRUNFLO, SUEDE CENTRALETHORSLUND P; WICKMAN FE.1981; NATURE (LOND.); ISSN 0028-0836; GBR; DA. 1981; VOL. 289; NO 5795; PP. 285-286; BIBL. 6 REF.Article

CHEMISTRY AND GEOCHEMISTRY OF SOLUTIONS AT HIGH TEMPERATURES AND PRESSURES: AN INTRODUCTION TO THE SYMPOSIUM = CHIMIE ET GEOCHIMIE DES SOLUTIONS A HAUTE PRESSION ET HAUTE TEMPERATURE: INTRODUCTION AU SYMPOSIUMWICKMAN FE; RICKARD D.1981; PHYS. CHEM. EARTH.; ISSN 0079-1946; GBR; DA. 1981; VOL. 13-14; PP. 1-8; BIBL. 7 REF.Conference Paper

GENERAL DISCUSSION = DISCUSSION GENERALERICKARD D; WICKMAN FE.1981; PHYS. CHEM. EARTH; ISSN 0079-1946; GBR; DA. 1981; VOL. 13-14; PP. 537-541Conference Paper

THE ISOTOPIC COMPOSITION OF GRAPHITIC CARBON FROM IRON METEORITES AND SOME REMARKS ON THE TROILITIC SULFUR OF IRON METEORITESDEINES P; WICKMAN FE.1973; GEOCHIM. COSMOCHIM. ACTA; G.B.; DA. 1973; VOL. 37; NO 5; PP. 1295-1319; BIBL. 1P.; 8 ILL.; 68 ANAL.Serial Issue

THE FLINK COLLECTION OF UNKNOWN LANGBAU MINERALS, A PROGRESS REPORT.MOORE PB; WICKMAN FE.1971; GEOL. FOEREN. STOCKHOLM FOERH.; SWE; 1971(5), VOL. 93, NUM. 0545, P. 289 A 301Miscellaneous

MOLYBDENITE POLYTYPES IN THEORY AND OCCURRENCE. 2. SOME NATURALLY-OCCURRING POLYTYPES OF MOLYBDENITE.FRONDEL JW; WICKMAN FE.1970; AMER. MINERALOGIST; USA; 1970, VOL. 55, NUM. 1112, P. 1857 A 1875Miscellaneous

WIDTH OF ALBITE TWIN LAMELLAE. PART 1. AN OLIGOCLASE FROM A PEGMATITE, BAMBLE, NORWAY.WICKMAN FE; LUNDSTROEM I.1969; LITHOS; NOR; 1969, VOL. 2, NUM. 0002, P. 197 A 213Miscellaneous

A CONTRIBUTION TO THE STABLE CARBON ISOTOPE GEOCHEMISTRY OF IRON METEORITES.DEINES P; WICKMAN FE.1975; GEOCHIM. COSMOCHIM. ACTA; G.B.; DA. 1975; VOL. 39; NO 5; PP. 547-557; BIBL. 17 REF.; 5 ILL.Article

NON-DESTRUCTIVE ACTIVATION ANALYSIS FLUID INCLUSIONS IN FLUORITE.WICKMAN FE; KHATTAB KM.1972; ECON. GEOL.; USA; 1972, VOL. 67, NUM. 0002, P. 236 A 239Miscellaneous

BLECKENSTAD, THE ONLY CALCARITE, IS A PSEUDOMETEORITE = BLECKENSTAD, LA SEULE CALCARITE, QUI EST UNE PSEUDOMETEORITEWICKMAN FE; UDDENBERG ANDERSSON A.1982; GEOLOGISKA FOERENINGENS I STOCKHOLM FOERHANDLINGAR; ISSN 0016-786X; SWE; DA. 1982; VOL. 104; NO 1; PP. 57-61; BIBL. 12 REF.Article

THE SUPPOSED METEORITE FALL AT OREBRO IN SWEDEN, 1958.WICKMAN FE; UDDENBERG ANDERSSON AG.1969; ARK. MINERAL. GEOL.; SWE; 1969, VOL. 4, NUM. 0006, P. 543 A 544Miscellaneous