作者:WANGJincao,XIABin,TANGJingru
摘要:The Lingtong-Jiaojia ore-centralized district is controlled by the tectonic stress field characterized bY the combination of extension and strike-slip, and the dip, dip angle, pitch and pitch angle of the ore bodies are all constrained by the dynamic conditions of the tectonics. The metallotectonic series for the ore-centralized district belong to the type of a combination of extension and strike-slip and can be subdivided into four sub-series. The ore-forming process in the brittle regime can be disintegrated into two stages, i.e., the embryonic fracture stage and the megascopic fracture stage, and ore-forming process is rather common in the ore-centralized district at the former stage. Moreover, several key structural patterns and their features were discussed and a preliminary assessment about the ore-forming prospect in this district was made in the paper.
發文機構:GuangzhouInstituteofGeochemistry InstituteofGeology
關鍵詞:山東地殼應力場成礦斷口分析金屬型地殼嶺隆金礦沉積焦家金礦沉積tectonic stress field characterized by a combination of extension and strike-slipmetallotectonic seriesore-forming embryonic fracture
分類號: P611[天文地球—礦床學][天文地球—地質學]P618.51[天文地球—礦床學][天文地球—地質學]