- 责任者：Li Zuochen (Key Laboratory of Western Mineral Resources and Geological Engineering ; Ministry of Education ; Chang’an University ; Xi’an 710054 ; China) ; Pei Xianzhi
- 刊名：Journal of Earth Sciences and Environment
- 出版年：2011
- 卷期：33(2)
- 关键词：沉积环境 ; sedimentary environment ; 早古生代 ; Lower Palaeozoic ; 南华纪 ; Nanhua Period ; 龙门山断裂带 ; Longmenshan Fault Zone
- 页码：p.117-124
- 图表：3 illus., 52 refs.
- 分类号：1200
- issnNo：ISSN1672-6561
- isbnNo：CN61-1423/P
Through the research on sedimentary strata of Nanhuan Period-Early Paleozoic of Back-Longmenshan tectonic belt in the northwest margin of Yangtze Block with the methods of petrology and sedimentary strata, the sedimentary and forming environments of Nanhuan Period-Early Paleozoic of Back-Longmenshan tectonic belt were discussed. The results indicated that the sedimentary environments of Nanhuan Period-Early Paleozoic of Back-Longmenshan tectonic belt could be divided into two stages, including the division-stable stage of Nanhuan-Sinian Period and the extension and division-collapse stage of Early Paleozoic; Back-Longmenshan tectonic belt had the repetitive process of divergence→lifting→partial divergence→lifting→divergence during the extension and division-collapse stage of Early Paleozoic; aulacogen sedimentary in Maoxian Group of Silurian System.