{"refrec":{"BRefID":302308,"RR":"<b>Reed, D.L.; Meyer, A.W.; Silver, E.A.; Prasetyo, H.</b> (1987). Contourite sedimentation in an intraoceanic forearc system: Eastern Sunda Arc, Indonesia. <i>Mar. Geol. 76</i>: 223-241. <a href=\"https://dx.doi.org/10.1016/0025-3227(87)90031-4\" target=\"_blank\">https://dx.doi.org/10.1016/0025-3227(87)90031-4</a>","BEntID":294552,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Mar. Geol. 76</i>: 223-241. <a href=\"https://dx.doi.org/10.1016/0025-3227(87)90031-4\" target=\"_blank\">https://dx.doi.org/10.1016/0025-3227(87)90031-4</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Reed, D.L.; Meyer, A.W.; Silver, E.A.; Prasetyo, H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Reed, D.L. <i>et al.</i>","Englishabstract":"Combined analyses of bathymetry, piston cores, 3.5-kHz echograms, and seismic reflection data reveal that sedimentation patterns in the eastern Sunda forearc are strongly influenced by vigorous deep- and bottom-water circulation. The affected region is located at the intersection of the Sumba Ridge and the Sawu-Timor Ridge, which together form a barrier to the outflow of Pacific Ocean Deep Water from the Sawu Sea to the eastern Indian Ocean. Bottom currents associated with the outflow have eroded a gap in the sill at a water depth of 1150 m, between the islands of Sumba and Sawu. Southwest of the gap, the widespread exposure of well-consolidated, middle Miocene to Pliocene foraminiferal chalks and oozes along the Sumba Ridge suggests that up to 1 km of overburden has been removed by the deep (1–1.5 km) currents. The eroded sediments have been subsequently deposited as muddy contourites in a thick (> 1km) sediment drift in the adjacent Sumba Basin. The drift consists of an elongated mound composed of reworked calcareous ooze and is bounded by moat-like channels. The influence of contour currents on trench-slope sedimentation can be significant and should be considered during studies of modern forearc systems and ancient subduction complexes on land.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Contourite sedimentation in an intraoceanic forearc system: Eastern Sunda Arc, Indonesia","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-17 01:32:22.649014","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1987,"MonPub":null,"DateUpdate":"2018-10-22","DateCreate":"2018-10-22","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:A1987J082200005","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/0025-3227(87)90031-4"},"refs":null,"anarec":{"AnaID":302308,"PubliDate":1987,"Pagination":"223-241","XtraPublOfAnaID":null,"ISBN":null,"Volume":"76","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43365,"SerRR":"Marine Geology. 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