流动构造（flow structure），是指岩浆在流动过程中所产生的构造。主要包括流线构造和流面构造两种。
在矿体的许多部位，异离体矿石表明有非常特征性的流动构造。
In many parts of the ore bodies the schlieren ore shows a very characteristic flow structure.
本文通过对摩挲营花岗岩体的流动构造研究，查明了岩浆侵位时流动空间的形态。
By the study of flow structures shown by orientated phenocrysts and some enclaves in Mosuoying Granite, the form of emplaced space of the magma is inferred.
岩墙群的构造形态和流动构造表明鲁西基性岩墙群是基性岩浆侵位到先存的张性破裂中的产物，岩墙自北部向南部侵入。
The flow structures and geometry evidences of the dykes indicate that the magma source of these dykes intruded the pre-existing tensional rupture.
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