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《Journal of Stratigraphy》 1992-03
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New contribution to the knowledge of the tectonic stratigraPhy of the “Longzhuagou Group”

Zhang Shi-hong,Shi Yang-shen and Wang Zhi-hong  
Palaeomagnetic and structural data suggest that the Longzhuagou Group should be divided into 2 series of sedimentary rocks, Shangyunshan formation and Kaibei formation, Both are predominantly marine. They were possibly formed at low latitude (15.1-23 N) and close relatively to the Nadanhada terrane. In contrast the predominantly coal bearing Peide and Zhushan formations were formed at high latitude (52.1-57.8N) and close relatively to the Jixi Group, which is the cover of Jiamusi terrane. During amalgamation of the terranes, the two kinds of strata were interlayened with each other structurally.
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