New TIMS U–Pb zircon dates constrain the magmatic history of ODP Holes 735B/1105A.
Hole 735B crust was formed over ≥0.214±0.032 Ma.
Dated samples become progressively younger with increased depth in the core.
The age-depth profile indicates each igneous series underplated the prior series.
Magmatic cooling rates were 103–104 °C/Ma from 900–700 °C.