Its geochemical feature indicates that ore forming elements mainly comes from stratum and rock of pre Devonian period and ore forming solution is complex fluid of syngenetic water, metamorphic water and meteoric water.
英
美
- 礦床的地質(zhì)地球化學(xué)特征表明，成礦物質(zhì)主要來(lái)自前泥盆紀基底的地層和巖石，成礦溶液主要為盆地同生水與變質(zhì)水及大氣降水的混合流體。
