A MULTIFACETED APPROACH TO DATE TECTONICALLY-DRIVEN EXHUMATION OF THE HIMALAYAN MIDDLE CRUST
The STD is an orogen-wide shear zone that exhumed high metamorphic-grade mid-crustal rocks in the footwall and juxtaposed them with low metamorphic-grade supracrustal rocks in the hanging wall. A sheared garnet-muscovite-biotite schist at the base of this ~1-km-thick shear zone contains pre-kinematic garnet that grew at ~600 °C and 900-1000 MPa between ca. 36 and 30 Ma. Garnet breakdown during decompression is inferred to have started at ca. 30 Ma from the increasing Y content of monazite. Syn-kinematic asymmetric Y-rich rims of monazite indicate the base of the STD was active from ca. 29 to <24 Ma at 600 °C based on quartz crystallographic <c>-axis preferred orientations fabrics. The schist yields an 18.8 ± 0.3 Ma white mica 40Ar/39Ar date, interpreted as a cooling age, which constrains the minimum age of ductile deformation at the base of the STD. A second white mica 40Ar/39Ar date from the upper part of the STD, which was deformed at lower temperature (<500 °C), is interpreted to indicate syn-kinematic recrystallization at 16 ± 2 Ma, suggesting that deformation propagated up-section within the shear zone.
These data constrain the onset of mid-crustal tectonically-driven exhumation along the STD to the early Oligocene, several m.y. before commonly reported values. The well-constrained duration of activity of the STD in western Nepal (ca. 30 to <16 Ma) is combined to published estimates of dip-slip displacement (150-200 km) to calculate long-term average creep rates of 1.1 to 1.4 cm/year.