{"refrec":{"BRefID":78253,"RR":"<b>Michaud, F.; Bourgois, J.</b> (1995). Is the Rivera Fracture Zone a transform fault as currently accepted? <i>C. r. Acad. sci., Sér. 2, Sci. terre planètes 321(6)</i>: 521-528","BEntID":73792,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":" <i>C. R. Acad. Sci., Sér. 2, Sci. Terre Planètes 321(6)</i>: 521-528","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Michaud, F.; Bourgois, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Michaud, F.; Bourgois, J.","Englishabstract":"Swath bathymetry (SeaBeam) along with available earthquake slip vectors suggest the existence of three distinct rectilinear segments along the Rivera Fracture Zone; these three segments trend differently instead of delineating a continuous smallcircle segment. Therefore, the Rivera Fracture Zone is not a transform fault as currently accepted but an accomodation zone between two diferent spreading systems. 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