摘要
Coalbed genesis study is the theoretical basis for coal geology and sedimentology. It has been suggested that the most economic coalbeds are formed in situ. However, the author discovered a large number of syndepositional slump coalbeds with main allochthonous components and associated gravity-influenced muddy interlayers for the first time in the extrathick coalbeds from the Fushun Basin, and established a new coal-forming model.
