au.\*:("WOLLIN G")
Results 1 to 11 of 11
Selection :
PLEISTOCENE CLIMATES IN THE ATLANTIC AND PACIFIC OCEANS : A COMPARISON BASED ON DEEP-SEA SEDIMENTS.ERICSON DB; WOLLIN G.1970; SCIENCE; USA; 1970(3), VOL. 167, NUM. 3924, P. 1483 A 1484Miscellaneous
SYNTHESIS OF PROTEIN, NUCLEOSIDES AND OTHER ORGANIC COMPOUNDS FROM CYANAMIDE AND POTASSIUM NITRITE UNDER POSSIBLE PRIMITIVE EARTH CONDITIONSWOLLIN G; RYAN WBF.1979; BIOCHIM. BIOPHYS. ACTA; NLD; DA. 1979; VOL. 584; NO 3; PP. 493-506; BIBL. 37 REF.Article
LATE PLEISTOCENE CLIMATES RECORDED IN ATLANTIC AND PACIFIC DEEP-SEA SEDIMENTS.WOLLIN G; ERICSON DB; EWING M et al.1971; IN: LATE CENOZOIC GLACIAL AGES; 1971, P. 199 A 214Miscellaneous
GEOMAGNETIC VARIATIONS AND CLIMATIC CHANGES 2,000,000 B.C. - 1970 A.D.WOLLIN G; ERICSON DB; WOLLIN J et al.1973; IN: METHODES QUANT. ETUDE VAR. CLIMAT PLEISTOCENE. COLLOQ. INT.; GIF-SUR-YVETTE; 1973; PARIS CNRS; 1973, VOL. 219, P. 273 A 288Miscellaneous
RELATIONSHIP BETWEEN ANNUAL VARIATIONS IN THE RATE OF CHANGE OF MAGNETIC INTENSITY AND THOSE OF SURFACE AIR TEMPERATUREWOLLIN G; RYAN WBF; ERICSON DB et al.1981; J. GEOMAGN. GEOELECTR.; ISSN 0022-1392; JPN; DA. 1981; VOL. 33; NO 10; PP. 545-567; BIBL. 2 P.Article
CLIMATIC CHANGES, MAGNETIC INTENSITY VARIATIONS AND FLUCTUATIONS OF THE ECCENTRICITY OF THE EARTH'S ORBIT DURING THE PAST 2, 000, 000 YEARS AND A MECHANISM WHICH MAY THE RESPONSIBLE FOR THE RELATIONSHIPWOLLIN G; RYAN WBF; ERICSON DB et al.1978; EARTH PLANET. SCI. LETTERS; NLD; DA. 1978; VOL. 41; NO 4; PP. 395-397; BIBL. 11 REF.; 1 ILL.Article
VARIATIONS IN MAGNETIC INTENSITY AND CLIMATIC CHANGES.WOLLIN G; ERICSON DB; RYAN WBF et al.1971; NATURE, G.B.; 1971(8), VOL. 232, NUM. 5312, P. 549 A 550Miscellaneous
MAGNETIC INTENSITY AND CLIMATIC CHANGES 1925-1970WOLLIN G; KUKLA GJ; ERICSON DB et al.1973; NATURE; G.B.; DA. 1973; VOL. 242; NO 5392; PP. 34-37; BIBL. 16 REF.Serial Issue
THE FLOOR OF THE OCEAN.MOORE JR; BASCOM W; EMERY KO et al.1971; IN: OCEANOGRAPHY.; 1971, P. 124 A 205Miscellaneous
