Paro Fm
Type Locality and Naming
Tethyan Himalaya.
Lithology and Thickness
"1–2 km-thick packages of fine-grained, thin-medium bedded quartzite separated by 10 –200 m-thick marble bands that are mappable across the entire exposure" (McQuarrie et al. 2013).
From Long et al. (2011; Legend to Geological map of Bhutan): Lower unit – Muscovite-biotite-garnet-staurolite schist, with kyanite present within quartz veins. Quartzite interbeds become more common upsection. 600 m-thick (Tobgay et al., 2010). Middle unit – Gray to tan, thin-bedded, fine-grained, micaceous quartzite, interbedded with biotite-garnet-muscovite schist, rare calc-silicate rocks, and marble. Contact with schist of lower unit is gradational. Two white to gray, medium crystalline marble marker beds (m1, 10 m-thick; m2, 100-200 m-thick) are divided out. 2,000 m-thick total (Tobgay et al., 2010). Upper unit – Tan to gray, very coarse-grained, thin- to medium-bedded, cliff-forming, biotite-rich quartzite, interbedded with biotite-muscovite-garnet schist. Marble marker bed (m3; 250 m-thick) is divided out. 1,600 m-thick total (Tobgay et al., 2010).
Relationships and Distribution
Lower contact
Unconformity onto Precambrian "Lower Greater Himalayan protoliths"
Upper contact
Uncertain – no details given (perhaps not exposed in mapped region?); but indicated that next younger regional unit would be either upper Pele La Gr, or Devonian-age Tang Chu Gr.
GeoJSON
Fossils
Age
Depositional setting
Additional Information