The stable isotopic composition of insoluble, refractory elements such as titanium (Ti) or zirconium (Zr), which are modified by magmatic differentiation but, a priori, poorly affected weathering diagenesis, serve powerful potential proxies to reconstruct the compositional evolution continental crust. Here we present Zr compositions (?94/90ZrIPGP-Zr, per mille deviation 94Zr/90Zr from IPGP-Zr s...