• 责任者：Xu Deru (Key Laboratory of Mineralogy and Metallogeny ; Guangzhou Institute of Geochemistry ; Chinese Academy of Sciences ; Guangzhou 510640 ; China) ; Wang Li
• 刊名：Geotectonica et Metallogenia
• 出版年：2011
• 卷期：35(4)
• 关键词：煤系 ; coal measures ; 江西 ; Jiangxi Province
• 页码：p.513-524
• 图表：9 illus., 2 tables, 26 refs.
• 分类号：1004
• issnNo：ISSN1001-1552
• isbnNo：CN44-1595/P

The formation of the Ping (Pingxiang)-Le (Leping) coal-bearing depression zone was strictly controlled by three-period and four-stages of tectonic-sedimentary evolution from Mesozoic to Cenozoic. These include Nappe-stage in Indosinian, basal-detachment and fold-thrust stage in the end of Late Triassic and cover strike-slip stage in the end of Early Jurassic, and cover and basal sliding stage during Himalayan. Thus, multistage conversion between sag and fault depression made the basin type of the Pingle depression showing different geotectonic features. As a result of this study, the authors establish a coal-controlling structural model which could be a guide for coal mine exploration in the Fengcheng region.