大水闸与青龙哨陆相磷块岩

大水闸磷矿和青龙哨磷矿是我国两个最重要的陆相磷块岩矿床,矿床规模大、品位高,是我国正在开采利用的重要磷矿基地中的两个磷矿基地。我们称这种陆相磷矿为“大水闸式磷矿”。该类陆相磷块岩是世界罕见的一种具有重大工业价值的新的磷矿类型,在磷矿分类中又增加了一个新的成员。

The Qinglongshao and Dashuizha Continental facies phosphorite

The Dashuizha phosphorus mine is located in a place where Shifang and Mianzhu of Sichuan Province meet and where the brecciated phosphorus ore is in lower part of the original "Shifang type" one. The original "Shifang type" phosphorus ore was mainly composed of the palingenetic marine phosphorite of Middle and Late Devonian Epoch including upper ore beds of goyazite (originally called sulfur goyazite ore ) and lower brecciated phosphorite. It was found by recent studies of the authors that the upper mineral bed of goyazite belongs to the marine facies phosphorite of Middle Devonian Epoch while the lower part brecciated phosphorite to the continental facies one whose geological characteristics are very similar to the Qinglongshao phosphorite ore of Yunnan Province. The phosphorus ore bed bearing goyazite and kaolinite were found to be in onlap unconfornity in the apical plate of the Qinglongshao brecciated phosphorite, which indicates the stratigraphic pattern and bed sequence of the Qinglongshao phosphorus ore are very similar to those of the Dashuizha ore. The present study has confirmed that both the brecciated phosphorite systems are continental facies and that the Meishucun phosphorite of the Lower Cambrian was weathered, accumulated, consolidated and so on for a long time from the Late Cambrian to Late Devonian. Thus, the Qinglongshao and Dashuizha phosphorus ores could be called the "Dashuizha type" phosphorus ore.