Abstract:The stratabound mineral deposits in the Kuandian Group (PtK) are all transformed deposits and might be classified into two types: syngenetic transformed deposits, such as boron, iron, rare-earth, pyrite and apatite ores, and metamorphic hydrothermal transformed deposits, such as magnesite, asbestos and talc. The boron deposits in the Kuandian Group are confined to the middle part of the Kuandian geosyncline 45 km in width and 400 km in length, constituting a boron ore zone trending in the same direction as the geosyncline itself. They may be classified commerrcially into two types, i. e., "white boron ore" and "black boron ore". The former, made up mainly of boronmagnesite and suanite, are rarely associated with ferruginous minerals, while the latter contains ludwigite and magnetite, forming ore of mixed type, the former occurs unexceptionally in PtK: while the latter can be found in three stratigraphic positions, i. e., PtK22, PtK41 and PtK62. The B-Fe-TR formation has formed in time and space a metallogenic sequence and three obliquely arranged zones on account of the uneven distribution of useful element composition in the original strata. Within the Kuandian geosyncline, therefore, three subformations could be recognized from its periphery in inward succession: Fe-TR, B-Fe-TR and B-(Fe) subformations, accompanied by an increase in B and a decrease in Fe. So far as economic significance is concerned, the iron deposits in the Kuandian Group are likely to be assigned to four types, namely, Fe-TR type (Shengtieling type), Fe-B type (Wengquangou type), Fe-rich and sulfide-bearing type (Yanglin type) and Fe-magnesite-magnetite type (Daankou type). The "sedimentation- transformed" idea ought to be emphasized in the whole process of mineral exploration for stratabound deposits in Kuandian Group except for metamorphic-hydrothermal-transformed ones. Sedimentationis the base of being transformed, which has been verified by years of survey and prospecting.
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姜春潮，刘光启.1983.宽甸群中的层控矿床[J].矿床地质,2(3):1~8.1983.On the stratabound mineral deposits in the Kuandian Group[J].Mineral Deposits2(3):1~8
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