commen mollusks, coral, coralline alaae, and benthic ferams (rotaline ard miliclid). Diagenesis has extensively altered strata near the atei! margin. Aragenite disscluticn and calcite cements (radiaxial and cloudy prizgmatic) are abiundast in fore-r2ef, reef, and same back-reef strata. Fetrogrephic ana gecchemical data indicate aragonite dissclutian and calcite cementatian ir seawater at buriel deoths ef 100 ta 300 m. Dolomite occurs in slope and deeply buried reefal carbonates. Mest delomitization occurred at burial depths of more than 1000 m in cool marine waters circulating through the atoll. iagconal etrata are rat significantly altered by marine diagenesis end still centain abundant primary aragonite and magnesium calcite. Record - 3 aPIGLOG File 193: > 16260861 EDB-89 3057142 Title: Bikini Atoll groundwater development Auther: Peterson, F.L. fFffiliaticons Univ. of Hawaii. denoelulu (USA) Conference Title: °3, annual meeting of the Geolcgical Siaciety cf America Conference Location: Grilande, FL. USA Conference Date: 29 Oct 1995 Serrce: Geel. Sec. Am., fostr. Programs (United States) v it. Date: 1995 687 p. Cocean: GAAFE Feoort Now: CONF-3510489Docunent Type: Journal Article: Cenference literature Lancesge: English Journal announcement: ETDASED SubTile: ETD ‘Eneray Technolegy Data Exchange); INS (US Atomindes tageti. TMT (PGE centractar) werk Location: United Sta tes Abstract: Nuclear weapons testing during the 1950's hae left the eo.1 and yreund water on Bivini 4teli contaminated with cesium-1397, and to a lesser 2xtaems, etrombiur-o0, Plans currentis, are underway fer the cleen-un and ese etilenest cf tre atell by removal cf approximately the upper 30 cm if B22, Rrry la:“ge-scale resettiement pregram must include prowpeiens fer vater supply. This will be achieved principaliy By catchment and storege af réin weter,. hewever, since rainfall in Bikini is highly seascnal and drougtts cccur frequently. ground water development must aiso be cxnsicered., The quentity o* petable ground water trat cen be developed is limited sy its salinity and radiclegical quality. The few ground water samples evailable from Bikini, which have beer collected from only about the top meter cf the groundwater beady, indicate that small bodies of potabie ground water exist on Bikini and Eneu, the two principal living iglands, but that cesium and strontium in the Bikioni ground water exceed drinking water stesdards. In order to make a reasonable estimate cf the Ground water develegment potential for the atoll, some 40 test borehcles will be drilled during July/August 1985, and a pregram cf water quality monitoring initiated. This paper will describe preliminary results of the driliing anc menitcring work. Fecord - 4 ADIA.GG File i922: 1513723 EDB-as:087080 Title: Streotium-isotope stratigraphy af Enewetak Atoll 9004632