{"refrec":{"BRefID":249649,"RR":"<b>Crowley, J.W.; Katz, R.F.; Huybers, P.; Langmuir, C.H.; Park, S.-H.</b> (2015). Response to Comment on “Glacial cycles drive variations in the production of oceanic crust”. <i>Science (Wash.) 349(6252)</i>: 1065-b. <a href=\"http://dx.doi.org/10.1126/science.aab3497\" target=\"_blank\">http://dx.doi.org/10.1126/science.aab3497</a>","BEntID":241352,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 349(6252)</i>: 1065-b. <a href=\"http://dx.doi.org/10.1126/science.aab3497\" target=\"_blank\">http://dx.doi.org/10.1126/science.aab3497</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Crowley, J.W.; Katz, R.F.; Huybers, P.; Langmuir, C.H.; Park, S.-H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Crowley, J.W. <i>et al.</i>","Englishabstract":"Goff comments that faulting is important for creation of abyssal hills and is the dominant process at slow-spreading ridges. We respond that faulting is indeed important but cannot alone explain the bathymetric signal predicted by our models and observed at the Australian-Antarctic Ridge. We show that for intermediate- to fast-spreading ridges, abyssal hill spacing is consistent with the periodicity of the obliquity cycle. 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