Experimental deformation of partially melted granite revisited: implications for the continental crust

Abstract A review and reinterpretation of previous experimental data on the deformation of partially melted crustal rocks reveals that the relationship of aggregate strength to melt fraction is non‐linear, even if plotted on a linear ordinate and abscissa. At melt fractions, Φ 0.07. This melt fraction (Φ = 0.07) marks the transition from a significant increase in the proportion of melt‐bearing grain boundaries up to this point to a minor increase thereafter. Therefore, we suggest that it is the increase of melt‐interconnectivity that causes the dramatic strength drop between the solidus and a melt fraction of 0.07. We term this drop the ‘melt connectivity transition’ (MCT). A second, less‐pronounced strength drop occurs at higher melt fractions and corresponds to the breakdown of the solid (crystal) framework. This is the ‘solid‐to‐liquid transition’ (SLT), corresponding to the well known ‘rheologically critical melt percentage’. Although the strength drop at the SLT is about four orders of magnitude, the absolute value of this drop is small compared with the absolute strength of the unmelted aggregate, rendering the SLT invisible in a linear aggregate strength v . melt‐fraction diagram. On the other hand, the more important MCT has been overlooked in previous work because experimental data usually are plotted in logarithmic strength v . melt‐fraction diagrams, obscuring large strength drops at high absolute strength values. We propose that crustal‐scale localization of deformation effectively coincides with the onset of melting, pre‐empting attainment of the SLT in most geological settings. The SLT may be restricted to controlling flow localization within magmatic bodies, especially where melt accumulates.