A film of pyrites was discovered on the interface of Lower Sinian Sidingshan Formation and Fengtai conglomerate , at Sishilichangshan Mountains in the south margin of the North China Block.
英
美
- 華北陸塊南緣四十里長(cháng)山地區下震旦統四頂山組疊層石白云巖與其上部鳳臺礫巖的接觸界面上為一薄層黃鐵礦,對其宏觀(guān)和微觀(guān)以及地球化學(xué)特征研究表明,這一接觸界面為裂離不整合。