摘要
The Lukuishan iron deposit was deposited from underground-water-derived ore solution, highly characteristic of underground.water ore deposition. The ore solution resulted mainly from squeezed Iiquids. The source beds seem to be the main source for iron-bearing materiah This deposit is strictiy controlled by palaeohydrogeological conditions and hydrogeochemical environment during the stage of ore deposition. In other words, this deposit was generally formed at the point where ancient underground water (i.e., the ore solution) discharged.
The Lukuishan iron deposit was deposited from underground-water-derived ore solution, highly-characteristic of underground-water ore deposition. The ore solution resulted mainly- from squeezed liquids. The source beds seem to be the main source for iron-bearing material. This deposit is strictly controlled by palaeohydrogeological conditions and hydrogeochemical environment during the stage of ore deposition. In other words, this deposit was generally formed at the point where ancient underground water (i.e., the ore solution) discharged.
出处
《地球化学》
CAS
1982年第4期384-392,共9页
Geochimica
