• 责任者：Zhou Yong (Institute of Sedimentary Geology ; Chengdu University of Technology ; Chengdu 610059 ; China) ; Li Xianghui
• 刊名：Acta Geologica Sichuan
• 出版年：2011
• 卷期：31(2)
• 关键词：岩相古地理 ; lithofacies paleogeography ; 古气候 ; paleoclimate ; 四川 ; Sichuan Province
• 页码：p.142-144
• 图表：3 illus., 9 refs.
• 分类号：0803
• issnNo：ISSN1006-0995
• isbnNo：CN51-1273/P

Study of sedimentary facies indicates that the Penglaizhen Formation in the National Woodstone Geopark, Shehong is composed of purple, purplish gray, grayish green mudstone, fine-grained arkose and siltstone which may be divided into lacustrine, fluvial facies and iron oxide soil. The lacustrine facies may be subdivided into deep lake, coastal and shallow lake subfacies and fluvial facies may be subdivided into channel, levee, crevasse-splay, floodplain subfacies. The sedimentary facies indicates a semiarid climate.