Static recrystallization and preferred orientation of phyllosilicates: Michigamme Formation, northern Michigan, USA

The Michigamme Formation of the Marquette District in Michiganʹs Upper Peninsula comprises a sequence of cleaved rocks of increasing metamorphic grade. Because metamorphism in the area occurred after cleavage formation, the rocks provide an opportunity to study preferred orientation development of phyllosilicates under conditions of static recrystallization. texture goniometry on samples from the greenschist-facies zone that were collected at varying distances from the bounding biotite-in and garnet-in isograds, shows that: (1) the preferred orientation of phyllosilicates is always parallel to the mesoscopic cleavage, and (2) the degree of preferred orientation of phyllosilicates improves as a function of increasing metamorphic grade (from <4 to >9 m.r.d.). Scanning electron microscopy on these samples shows that: (1) the length/width ratio increases with increasing grade, and (2) grain shapes are better defined with increasing grade. us work on slates showed mechanical processes dominate at very low-grade metamorphism, whereas chemical processes are favored at higher grades. The Michigamme samples show that improvement of preferred orientation occurrred by grain dissolution and crystallization. Noncleavage-parallel phyllosilicate grains were preferentially dissolved, probably facilitated by internal strain energy from mineral defects, aided by chemical energy, whereas cleavage-parallel phyllosilicates were hosts for new growth along their basal planes. These results show that significant fabric strengthening can be achieved by grain dissolution and crystallization in the absence of tectonic stress.