ferrous carbonate meaning in Chinese

碳酸亚铁

With the intermittent activity of hot fluid containing cc ^ , ferrous carbonate minerals dissolved and precipitate repeatedly many times . in addition , dissolution of shells and feldspars , decrease of chlorite and increase of kaolinite could be found
随着富co _ 2热流体多次间歇性入侵导致了含铁碳酸盐矿物的反复多次溶解和沉淀、生物介壳大量溶蚀和长石铸模孔的形成以及绿泥石消失、高岭石增加等。
On the contrary , the reservoirs that were not influenced by hot fluid just were in early diagenetic stage b . 2 . based on the synthetic analysis of varied data , the mechanism of repeated dissolution and precipitation of ferrous carbonate minerals has been discussed
在进行充分的岩石学研究基础上，利用电子探针、稳定同位素及包裹体分析数据，探讨了异常成岩演化储层中含铁碳酸盐矿物反复溶解和沉淀的机理。