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- W88396899 abstract "Basement morphology and sediment distribution with the Yucatan Basin, Caribbean Sea, suggest that it formed as a rift basin. The age of rifting, as determined from heat flow and subsidence measurements is Early Tertiary. Analyses of multichannel and single channel seismic profiles crossing the basin show that it is underlain by a SW-NE trending, rectangular deep which extends the length of the basin and which is flanked to the NW and SE by topographic rises cut by SW-NE trending grabens. Seismic refraction and reflection and gravity profiles all suggest that the deep is floored with oceanic crust. Both deep and rise are transected by several NW-SE trending lineaments interpreted to be traces of transform faults. The rises are covered with acoustically layered sediments deposited during graben formation and overlain with thin, acoustically transparent sediments which postdate faulting. The deep is filled with flat lying, undeformed acoustically layered sediments which onlap all basement structure. Lack of a precise rifting age precludes establishing the exact relationship of basin opening to he Antilles-Cuban collision. The nature of the basin, its approximate age, and the tectonics of the region all suggest, however, the basin formed after the Cuban collision as Caribbean plate motion readjustedmore » from northward to eastward.« less" @default.
- W88396899 created "2016-06-24" @default.
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- W88396899 date "1985-01-01" @default.
- W88396899 modified "2023-09-23" @default.
- W88396899 title "Morphology of the Yucatan Basin: implications as to its origin and age" @default.
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