You, Chen-Feng; Chan, L.-H.; Gieskes, J. M.; Klinkhammer, Gary P. (American Geophysical Union, 2003-11-13)
Large-scale lateral advection of seawater within the
oceanic crust is thought to be the cause of low heat flow in
the Equatorial Pacific. Until now supportive evidence is
limited to reversals of B and δ¹¹B, Ca, Mg, SO ...