INSIGHTS INTO THE TECTONIC DEVELOPMENT OF THE WET MOUNTAINS, SOUTHERN COLORADO: INTERPRETING PROTOLITHS AND TEXTURES.
This study performed a detailed petrographic and textural analysis of amphibolites and amphibole biotite gneisses from the southern Wet Mountains. The amphibolites are typically well foliated and composed of hornblende and plagioclase with minor biotite and quartz, representing metabasites. The amphibolite biotite gneisses are strongly foliated, with well-developed quartz-rich domains and biotite-, amphibole- and plagioclase-rich domains. As the amphibolite and biotite are in apparent equilibrium, the mineralogy indicates an intermediate igneous protolith. All samples indicate deformation with undulose extinction and deformation twinning. One amphibole biotite gneiss sample contains a vein, which in 2D, is non-continuous, partially cutting some grains and fully cutting others. It is mostly infilled with quartz and biotite and where it contacts amphibole, these grains are partially or wholly replaced by biotite. All together, these data provide evidence for active subduction during formation of the protoliths, likely ~1.7 Ga, followed by burial and peak metamorphism during the Picuris Orogeny (~1.4 Ga). The textures indicate that peak deformation postdated peak metamorphic conditions. The Wet Mountains provide insights into the complex tectonic history during the development of Laurentia.