摘要
1.Objectives The Mohe Basin in Heilongjiang,China has a NEE thrust nappe belt,which was assembled by the root zone,middle thrust zone and thrust front,north-south and north-east normal faults with three tectonic activities of the Middle Jurassic to. Eocene,the Miocene,and the Early to Middle Pleistocene. The middle thrust zone and thrust front has a large number of folds,thrust faults,fractures and glutenites,which are the major structures of gas hydrate accumulation in the Mohe Basin.
