The rocky silicification in fault zone is controlled by various tectono-geochemical agencies:the dynamo-differentiation and chemical affinity,the dynamothermal meta- morphism and diaphthorisis,the oxidation and reduction,the hydrolysis and dewatering.
英
美
- 斷裂帶巖石的硅化現象是受組成巖石的化學(xué)元素的構造地球化學(xué)作用所制約的,包括動(dòng)力分異和化學(xué)親和作用,動(dòng)熱變質(zhì)作用和退化變質(zhì)作用,氧化和還原作用以及脫水和水解作用。
