The Upper Permian Xuanwei Formation widely occurs in western Guizhou,unconformably overlying the Emeishan basalts,and mainly consists of black shales.It is～170 m thick at Cuyudong Village,Weining County,West Guizhou,China,where the samples of black shale and sandy shale were collected and analyzed.The shales mainly contain SiO2,18.9%?44.1%,Al2O3,14.8%?52.8%,Fe2O3,1.0%?41.2%,LOI,3.2%?21.1%,TiO2,1.0%-6.7%,and MgO,0.2%?2.5%.The contents of all other major elements are lower than 1.0%.It is shown that the black shales have higher contents of Fe2O3 and LOI than normal shales.The siderites occurred in the black shales with higher contents of Fe2O3,which may be attributed to hydrothermal activities on seafloor.All analyzed shale samples have extremely high Ga,47.8×10-6-109.9×10-6(70.5×10-6 on average),higher than the industrial mining standard of Ga Resource Industry Standard.The total contents of rare-earth elements(REE) of 9 black shale samples vary from 213×10-6 to 1460×10-6,suggesting that these black shales are enriched in REE.The shale-normalized REE patterns display both positive and negative Ce anomalies(Ce/Ce* from 0.5 to 1.7),revealing that the Xuanwei shales were precipitated under oxic and anoxic conditions.The Rb-Sr chronological diagram of 6 shale samples in the Xuanwei Formation shows an age of 255±12 Ma.Strontium isotopic ratios(87Sr/86Sr)t0 range from 0.70635 to 0.70711,suggesting that these Xuanwei black shales might be derived from chemical weathering of the Emeishan basalts. The Upper Permian Xuanwei formed vast occurs in western Guizhou, unconformably overlying the Emeishan basalts, and mainly consists of black shales. It is ~ 170 m thick at Cuyudong Village, Weining County, West Guizhou, China, where the samples of black shale and sandy 44.1%, Al2O3, 14.8%? 52.8%, Fe2O3, 1.0%? 41.2%, LOI, 3.2%? 21.1%, TiO2, 1.0% -6.7% and MgO, 0.2%? 2.5%. The contents of all the major elements are lower than 1.0%. It is shown that the black shales have higher contents of Fe2O3 and LOI than normal shales. The side events occurred in the black shales with higher contents of Fe2O3, which may be attributed to hydrothermal activities on seafloor. All analyzed shale samples have an extremely high Ga, 47.8 × 10-6-109.9 × 10-6 (70.5 × 10-6 on average), higher than the industrial mining standard of Ga Resource Industry Standard.The total contents of rare-earth elements (REE) of 9 black shale samples vary from 213 × 10-6 to 1460 × 10-6, suggest ing that these black shales are enriched in REE. The shale-normalized REE patterns display both positive and negative Ce anomalies (Ce / Ce * from 0.5 to 1.7), revealing that the Xuanwei shales were precipitated under oxic and anoxic conditions. The Rb- Sr chronological diagram of 6 shale samples in the Xuanwei Formation shows an age of 255 ± 12 Ma.Strontium isotopic ratios (87Sr / 86Sr) t0 range from 0.70635 to 0.70711, suggesting that these Xuanwei black shales might be derived from chemical weathering of the Emeishan basalts.