Order number 940330-160606-96 -001-001 page 38 set 11 with 111 of 111 items Islands. The authors exposed modified Panasgnic-802 thermoluminescent dosimeters (TLDs) in over?100 sites for six months to accomplish this task. The sites were selected to be either in areas of known high gamma dose rates, in areas where the Marshallese would likely spend most of their time upon resettlement, or in areas where experimental environmental changes has been made. Therefore, the beta and gamma does rates do not represent island averages. The mean beta dose rate on Enue ranged from 23 mrem/yr at 1 cm to 6 mrem/yr at 100 cm, aS compared with a mean deep dose rate of 17.5 mrem/yr. The mean beta dose rate around houses and in general area on Bikini ranged from 425 mrem/yr at 1 cm to 178 mrem/yr at 100 cm, compared with a deep dose rate of about 154 mrem/yr. Because monitoring sites were specifically placed in the most-contaminated areas of Bikini and Eneu, the unshielded beta dose rates reported provide an upper limit of radiation dose;actual doses received by the Bikinians would be reduced significantly by clothing, footwear, and ground cover such as crushed coral, which reduces the beta dose rate by 80-90%. The amount of time spent in houses and in the minimally contaminated areas around houses and the lagoon would further reduce the beta dose rates reported here. 17 referenced, KEYWORDS 12 figures, 1 table. BIKINI/radiation monitoring ;CESIUM 137/beta dosimetry ; STRONTIUM 90/beta dosimetry SURFACE CONTAMINATION EDB Item 52 TITLE ENGLISH PERSONAL AUTHOR PUB. DATE (YYMMDD) LIMITATION CODE ABSTRACT ;BIKINI;PROGRESS REPORT; Evolution of reef and atoll margin carbonates, upper Eocene through lower Miocene, Enewetak, Marshall Islands Saller, A.H.;Schlanger, S.O. 880000 UNL Two wells drilled along the margin of Enewetak Atoll penetrated approximately 1,000 m of upper eocene, Oligocene, and lower Miocene carbonates. STrontium isotope stratigraphy indicates relatively continuous deposition of carbonate from 40 Ma to 20 Ma. Depositional environments show a gradual basinward progradation of facies with slope carbonates passing upward into fore-reef, carbonates. reef, back-reef, and~-agoonal Slope strata contain wackestones and packstones with submarine-cemented lithoclasts, coral, coralline algae fragments, benthic rotaline forams, planktonic forams, and echinoderm fragments. Fore-reef strata are dominantly packstones and boundstones containing large pieces of coral, 9003412 abundant benthic