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《Contributions To Geology and Mineral Resources Research》 1991-02
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Na SOURCE OF ALBITIZATION IN NINGWU-TYPE IRON-SULFUR DEPOSITS OF NINGWU-LUZONG AREA

Hu Wenxuan;Hu Shouxi Department of Earth Sciences, Nanjing University  
It is believed that Na source of albitization in Ningwu type iron-sulfur deposits is derived frommiddle Triassic marine anhydrite beds. This paper considers the point doubtful, because there is notonly no halite (NaCl) beds, but also less other form sodium in the anhydrite-bering sequence. So it isimpossible for anhydrite beds to be main Na source of albitization. Based on studies of many aspects of geology and geochemistry, authors believe that main sourceof albitization is from high-saline brines in contemporary volcanic depressions. Main evidences are asfollowings: 1) Alteration (albitization) and mineralizations are mainly located in the depressions or attheir margins, and clearly controlled by water-bearing depressions; 2) Under arid-evaporate condi-tions, the depressions concentrated many brines enriched in sodium, having material base of Nasource; 3) H-O isotope composition is near to the atmospheric water line, showing that ore-bearing so-lutions mainly derived from surface water and/or ground water-Na-rich brines in the depressions.Rb-Sr and S isotope data also support this viewpoint; 4) It has been proved that most ore depositsformed in hot-water circulating system. Similarly, in this area circulating systems caused by calderaand subvolcanic rocks make Na-rich brines permeate downwards and react with volcanic rocks, result-ing in a series of alterations (such as albitization) and mineralizations.
【Fund】: 博士后科学基金
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