{"refrec":{"BRefID":77553,"RR":"<b>Gamboa, L.A.P.; Rabinowitz, Ph.D.</b> (1981). The Rio Grande fracture zone in the western South Atlantic and its tectonic implications. <i>Earth Planet. Sci. Lett. 52(2)</i>: 410-418. <a href=\"https://dx.doi.org/10.1016/0012-821X(81)90193-X\" target=\"_blank\">https://dx.doi.org/10.1016/0012-821X(81)90193-X</a>","BEntID":73106,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Earth Planet. Sci. Lett. 52(2)</i>: 410-418. <a href=\"https://dx.doi.org/10.1016/0012-821X(81)90193-X\" target=\"_blank\">https://dx.doi.org/10.1016/0012-821X(81)90193-X</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Gamboa, L.A.P.; Rabinowitz, Ph.D.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Gamboa, L.A.P.; Rabinowitz, Ph.D.","Englishabstract":"A broad zone of linear, mappable basement structures is observed north and northeast of the Rio Grande Rise in the South Atlantic Ocean. These structures lie along the same flow line as the Sao Paulo Ridge, the Florianopolis High, and onshore lineaments, suggesting that they all comprise the same tectonic trend: the Rio Grande fracture zone. 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