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《Acta Sedimentologica Sinica》 2003-04
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Ice-frozen Sedimentary Structures and Their Significance for Environment in the Yellow River Delta

XIAN Ben zhong 1 JIANG Zai xing 1 HU Shu yi 1 CHU Bao jie 2 SONG Xiu xian 2 1(College of Geological Resource and Information, University of Petroleum, Dongying, Shandong 257061) 2(Institute of Geochemistry in Guangzhou, Chinese Academy of Science, Guangzhou 510640)  
Ice formed sedimentary structures, like water formed ones, are also abundant and characteristic in nature. Ice formed sedimentary structures can be divided into two categories, i.e. ice frozen sedimentary structure and ice molten one according to the factors controlling their formation. Observations of some points in field and laboratory simulation with sediments and water from Yellow river are used in this paper to describe the characters and origin of ice frozen sedimentary structures. Six sedimentary structures, ice split seams, ice slid marks, ice collapsed seams, ice induced pellets, ice eroded ripple marks and ice level marks, are newly found in Yellow River delta. Observations show that ice split seams and ice level marks, most widely distributed, have something to do with growth of ice crystals, that ice collapsed seams and ice slid marks, more partly distributed, are formed by the collapse and slippage of ice beds, that ice induced pellets are formed by ice splitting action and ice carrying particles action, and ice eroded ripple marks are the results from strong reworking of ice to old ripple marks. Distinguishing and environment interpretation of ice frozen sedimentary structures in Yellow River delta and Maershan member of Laiyang formation in Jiaolai basin suggest that the existing of ice frozen sedimentary structures is the important indication for the seasonal frozen soil ( the temperature about ±0℃) and sedimentary settings of riverbed, delta, flood land or tidal flat.
【Fund】: 山东省自然科学基金重点项目 (Z2 0 0 1E0 1 );; 国家重点基础研究发展规划项目 (G1 9990 7550 7)资助
【CateGory Index】: P512.2
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