Based on the distribution of metallogenic and associated elements in strata, rocks, ores and minerals of the ore district, the primary halos of the deposit, the sulfur and lead isotope compositions of the ores, and retios of elements re flecting environmental characteristics, combined with geological setting of the deposit, this paper summarizes the geological-geochemical environment for the formation of rocks, ores and halos, the material sources for mineralization and behaviours of late-stage hydrothermal elements,indicating evidently that this deposit is of stratabound type dominated by sedimentary enrichment.
出版日期: 1987-02-24
引用本文:
刘崇民, 徐外生. 北山铅锌黄铁矿矿床成因的地球化学论据[J]. 物探与化探, 1987, 11(1): 31-37.
Liu Chongmin, Xu Waisheng. GEOCHEMICAL GROUNDS FOR GENESIS OF THE BEISHAN Pb-Zn-PYRITE DEPOSIT. Geophysical and Geochemical Exploration, 1987, 11(1): 31-37.