Abstract:The first member of Guanghua formation, developed in Taigu Mountain area, is a set of normal pyroclastic sedimentary rocks. Based on the rock association, fabrics, vertical variation and the changes of sedimentary environment of the area, one second-order sequence can be recognized, including 2 third-order sequences with 7 fourth-order sequences. The study on the sequence stratigraphy may support the research on the sequence strata of Mesozoic continental basin in Daxinganling region.
李伟, 毕中伟, 付俊彧. 内蒙古阿荣旗太古山早白垩世光华组一段沉积岩层序地层特征[J]. 地质与资源, 2011, 20(2): 124-127.
LI Wei, BI Zhong-wei, FU Jun-yu. SEQUENCE STRATIGRAPHY OF THE FIRST MEMBER OF GUANGHUA FORMATION, EARLY CRETACEOUS IN TAIGU MOUNTAIN AREA, INNER MONGOLIA. GEOLOGY AND RESOURCES, 2011, 20(2): 124-127.