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断裂构造地球化学是研究断裂作用与其有关的物质组分之间的相互关系。F_4断层系张性为主的并带有剪性的断层,发育在碳酸盐岩岩石中。在断层作用过程中,断层中心的构造岩,即所产生的角砾岩,相对于旁侧的岩石,在岩石化学成分上,富集了F_2O_3、FeO、MnO和Al_2O_3,而贫化了K_2O。其中Fe_2O_3量多于FeO量;在微量元素上,富含Nj、W、Pb、Zn、Sb,而Cr、Ti的含量则显得比较低。而整个断层构造岩,在成分上的最大特点是带出了Mg,而带入了Ca。
Fault tectonics Geochemistry is the study of the relationship between the fracture component and its associated material components. F_4 Fault-dominated and scotomast faulting, developed in carbonate rocks. In the process of fault faulting, the tectonic rocks in the center of faults, that is, breccias produced, are enriched in the chemical compositions of rocks with F_2O_3, FeO, MnO and Al_2O_3 and depleted in K_2O. Among them, the amount of Fe 2 O 3 is more than that of FeO. The content of trace elements is Nj, W, Pb, Zn and Sb, while the content of Cr and Ti is relatively low. The whole fault structure rock, the most prominent feature in the composition is brought out of Mg, which brought Ca.