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BULLETIN OF TIlE GEOLOGICAL SOCIETY OF CIlINA Vol. XXVIII, pp. 65-69, 3 Figs., Jun. 19'ê8 On a Layer of Grossularite, Epidote and Calcite, Occurring at Kumush, Roso, Sinkiang* By S. H. Stnic and S. C. KWAN (Geological Survey of China) With 3 Tct-figure INTRODUCTION In March, 1944, while carrying on the geological reconnaissance in the Hosot-Tokson2 area, the writers had an opportunity of spending a few days in the vicinity of a small village named Kumush3 (Fig. 1) to study a moderately metamorphosed rock series. This region is characterized by Tihwa Dapancheng 0 50 iookm Tohson H.so Koroshar Kuus: 'OSinger Fig. 1 Map showing the location of (x)gmssularite and epidote gentle slopes and open valleys, thus attaining a topographic maturity and laying bare a wide region of bed rocks. About half a kilometer noith of ICumush, a layer of grossularite, epidote, calcite and other minor minerals was found. It occurs as a rather uniform layer in the porphyroblastic schist of the metamorphosed rock series which contains abundant red pegmatitic intrusives. Striking approximately E-W with a dip of 800 southward in accordance with the schists, this layer reaches more than 75 cm in thickness *Rejv«l for publication on February 26th.
Acta Geologica Sinica (English Edition) – Wiley
Published: Jun 1, 1948
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