SEDIMENTARY STRATIGRAPHY AND MORPHOLOGY OF THE ANCIENT WRECK AREA IN HEZE, SHANDONG PROVINCE
HUANG Wen-feng1, SUN Ming2, FENG Chao-chen3, GUO Shi-chun1
1. Heze Mineral Resources Exploration and Development Center, Heze 274000, Shandong Province, China; 2. Mudan District Institute of Cultural Relics and Protection, Heze City, Heze 274000, Shandong Province, China; 3. South Shandong Institute of Geo-engineering Exploration, Yanzhou 272100, Shandong Province, China
Abstract：The sedimentation stages in the ancient channel of Zhaowang River are obvious. During the early stage, the sedimentation is mainly medium-fine sand and silty sand, with shifting sedimentary rhythm. The sediments in the late stage are dominated by silty fine sand and silty sand. From the bottom of the sunken ship upward, two sediment sections can be recognized, namely, flood deposition and channel deposition, with grain sizes getting finer. Analysis for the profile of channel sedimentation shows horizontal swings. After the ship had collided to the point bar and sunken, the braided channels disappeared gradually, when the area near the wreck started to accept a stable channel deposition.
黄文峰, 孙明, 冯超臣, 郭世春. 山东菏泽古沉船地区沉积地层和地貌研究[J]. 地质与资源, 2011, 20(4): 312-315.
HUANG Wen-feng, SUN Ming, FENG Chao-chen, GUO Shi-chun. SEDIMENTARY STRATIGRAPHY AND MORPHOLOGY OF THE ANCIENT WRECK AREA IN HEZE, SHANDONG PROVINCE. GEOLOGY AND RESOURCES, 2011, 20(4): 312-315.
2011, Vol. 20 
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