含铁建造或含铁层位，多产于海进序列的岩石中。
Iron formations or iron-bearing strata occurred in the rocks of transgression sequence.
含铁建造与沉积旋回在时空和物源上存在着密切的成因联系。
The close relation of origin is shown between the iron-formation and the sedimentary cycle in time, space and compositional source.
前寒武纪条带状含铁建造铁矿床分为阿尔戈马型和苏必利尔湖型两大类。
Precambrian BIF iron ore deposit can be divided into two types, Algoma-type and Lake Superior-type.
该矿床属于受含铁沉积建造及变质作用控制的变质沉积型矿床。
This deposit belongs to metamorphic sedimentary type which is controlled by iron-bearing sedimentary construction and metamorphism.
该矿床属于受含铁沉积建造及变质作用控制的变质沉积型矿床。
This deposit belongs to metamorphic sedimentary type which is controlled by iron-bearing sedimentary construction and metamorphism.
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