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    Geological indications for young horizontal displacements in the Central Rhenish Massif
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    and complex are the two basic forms of the association of granitoid. This is also a general character of granitoid geology in south China. Compound massif means a that is spatially associated with several granitoid rocks at different ages. Thus the granitoid components are not geneticaly related with each other. The complex massife is meant to a that is associated with multiply differentiating ascending and emplacing magma from the same chamber. It is theoretically and pratically important to distinquish the two kinds of massifs.
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