1)  lithification,lithifaction
岩化
2)  Dolomitization
白云岩化
1.
This study shows that dolomitization in the area studied is characterized byrepeatedly superimposition.
在岩石学研究的基础上，运用稳定同位素、微量元素、X射线衍射、阴极发光、扫描电镜及流体包裹体等技术和方法，对鄂尔多斯盆地东部下奥陶统白云岩进行综合研究表明，区内白云岩化具多期叠加的特点。
3)  fenitization
霓长岩化
4)  Formalization
云英岩化
5)  migmatization
混合岩化
1.
The upper is silicified zones which contains breccias in serious size; The lower is migmatization rocks which incorporating brittle.
文章中主要描述了南雄断裂带构造岩的特征,其岩石可以分为两段,上段为硅化带岩石,含有大小不等的角砾,强烈硅化;下段为混合岩化岩石,残斑碎裂,岩石发生脆性形变。
2.
The zircon U-Pb age suggests that there was a migmatization during the Yanshan Period, w.
锆石Ｕ－Ｐｂ定年结果表明，在大别杂岩内存在燕山期的混合岩化作用，其时代为（１２９。
6)  mylonitization
糜棱岩化
1.
It is considered that the mylonitized alkaline granite is of sedimentary-metamorphic genesis in view of the following facts: bedding is exhibited in the rocks, before mylonitization the rocks had granoblastic texture and rock-forming minerals such as natro-griinerite, which reflect region metamorphic genesis, and the zircons.
本文在野外工作基础上,系统研究了云南大平糜棱岩化碱性花岗岩岩石结构构造、矿物组成、主微量元素和锆石特征等。
2.
The mylonitization occurred in about 353- 370Ma ago with the temperature ranging from 425℃ to475℃ and pressure 3.
并论证了相应的糜棱岩化作用发生在353～370Ma前。
参考词条
补充资料：云英岩化
分子式：
CAS号：

性质：形成以白云母和石英为主要成分岩石的高温热液蚀变作用。常发生在花岗岩类侵入体中，由岩浆期后富水、硼、氟等挥发分和钾、硅的高温流体作用于酸性围岩而形成。矿物成分除白云母，石英以外常见有萤石、黄玉、锂云母、电气石等。并共生有钾长石化和钠长石化作用。云英岩多呈脉状产出，共生有云英岩型矿床，如黑钨矿、白钨矿、绿柱石、锂云母、锡石、辉钼矿以及铌、钽、稀土等。

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