au.\*:("EDSALL DW")
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TRACE ELEMENTS IN TEPHRA AS INDICATORS OF MAGMATIC COMPOSITION IN THE ALEUTIAN ARC.EDSALL DW.1976; GEOL. SOC. AMER., BULL.; U.S.A.; DA. 1976; VOL. 87; NO 9; PP. 1269-1272; BIBL. 19 REF.; 7 ILL.; 16 ANAL.Article
MID-PLATE TEPHRA, EOCENE TO RECENT; HAWAII.EDSALL DW.1975; GEOL. SOC. AMER., ABSTR. PROGRAMS; U.S.A.; 1975, VOL. 7, NUM. 0007, P. 1064 A 1065Miscellaneous
ECONOMY IS NOT A MAJOR BENEFIT OF CLOSED-SYSTEM ANESTHESIAEDSALL DW.1981; ANESTHESIOLOGY; ISSN 0003-3022; USA; DA. 1981; VOL. 54; NO 3; PP. 258; BIBL. 1 REF.Article
DISTRIBUTION AND SIGNIFICANCE OF PLEISTOCENE SHORELINE FEATURES ON THE CONTINENTAL SHELF OF THE EAST COAST OF THE UNITED STATES.EDSALL DW.1977; IN: 10TH INQUA CONGR. ABS.; BIRMINGHAM; 1977; NORWICH; GEO ABS.; DA. 1977; PP. 123Conference Paper
GEOLOGIC DEVELOPMENT OF CENOZOIC CONTINENTAL MARGIN OF SOUTHEAST GEORGIA EMBAYMENT.EDSALL DW; DILLON WP.sdIN: AM. ASSOC. PET. GEOL. SOC. ECON. PALEONTOL. MINERAL. MEET.; WASHINGTON, D.C.; 1977; S.L.; DA. S.D.; PP. 92Conference Paper
MORPHOLOGY AND EVOLUTION OF THE SOUTH CHINA SEA.(ABSTRACT).EDSALL DW; GEDDES WH; HEEZEN BC et al.1968; GEOL. SOC. AMER., ABSTR. PROGRAMS; USA; 1968(11)Miscellaneous