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Results of velocity-cycling tests
(a-b) indicates steady-state sliding was reached during the intercycle period, so that an a-b value could be obtained by inverse modeling (see Table S4). -
Primary seismic horizons of Maurice Ewing Line 41, IODP Site 381-M0078
Two options for choosing a horizon position are the peak of seismic reflection amplitude and the preceding zero or first break two-way traveltime (TWT). U = seismic unit... -
Primary seismic horizons of Maurice Ewing Line 41, IODP Site 381-M0079
Two options for choosing a horizon position are the peak of seismic reflection amplitude and the preceding zero or first break two-way traveltime (TWT). U = seismic unit... -
Primary seismic horizons of Maurice Ewing Line 22, IODP Site 381-M0080
Two options for choosing a horizon position are the peak of seismic reflection amplitude and the preceding zero or first break two-way traveltime (TWT). U = seismic unit...
