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本文阐述了苏皖南部层控断裂在动力成岩成矿过程中杂岩的发育特征,指出这是研究断裂成岩成矿作用的重要途径。此外,作者以I.普里高津(Prigogine)的耗散结构学说,初步探讨了杂岩的发育机制。
This paper describes the developmental characteristics of bedding rocks in the southern part of Jiangsu and Anhui provinces during dynamic diagenesis and mineralization, and points out that this is an important way to study the mineralization of fractures. In addition, the authors initially discussed the mechanism of the development of complexes with the theory of dissipative structure of Prigogine.