The black shale of Niutitang formation of Lower Cambrian in Guizhou province is widespread, thick, high in organic content and formed in anaerobic, euxinic and stagnant marine environment, with reserves of about 1 960× 10^8 m^3. The multi-episode tectonic movements and thermal events resulted in its complex occurrence and partial micro-metamorphism, but the black shale still has certain of shale gas po-tentials in it, deserving to make further studies. It is suggested that in the future geological exploration and development of shale gas should consider the black shale, tight elastic rocks and carbonate rocks and their reservoirs in Guizhon.
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