摘要
The authors discussed the metallogenic conditions of goldbearing skarn deposits along the middlelower Yangtze River reaches. Gold was enriched in mantleoriginated magmas while copper was enriched in crustoriginated magmas. So the enrichment of gold in skarn deposits was decided by the M/C ratios of the intrusive rocks. The distribution of these deposits was controlled not only by the localization of the intrusive rocks which were decided by Mesozoic Eradeveloped largescaled and deepseated faults, but also by the favorable stratigraphic horizons.
