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Guo YONGSHENG,HAN YOUSONG,YANG GUANGFU,ZHANG MINGHAN. 1984. DISCUSSION ON THE PLEISTOCENE HIGH SEA LEVEL ABOUT THE SHANDONG PENINSULA. Acta Oceanologica Sinica, (2):238-245
DISCUSSION ON THE PLEISTOCENE HIGH SEA LEVEL ABOUT THE SHANDONG PENINSULA
DISCUSSION ON THE PLEISTOCENE HIGH SEA LEVEL ABOUT THE SHANDONG PENINSULA
Received:May 08, 1982  Revised:August 15, 1983
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Author NameAffiliation
Guo YONGSHENG Shandong Normal College, Jinan 
HAN YOUSONG Institute of Oceanology, Academic Sinica, Qingdao 
YANG GUANGFU Institute of Oceanology, Academic Sinica, Qingdao 
ZHANG MINGHAN Institute of Oceanology, Academic Sinica, Qingdao 
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Abstract:
      It has for many years been controversial whether there was a Pleistocene high sea level on the Shandong Peninsula. Our investigations in recent years suggest that the red sandy sediments distributed around the Yuanyaodun village, Weihai County, the "Liukuang Red Bed" and the loess-like deposits near Penglai County should be terrestrial deposits, and there is will not a convincing evidence to confirm that abrasion landforms found above the 10m elevation oa the coast are of marine origin. From these, it is still not safe to say that a high sea level had occurred in the Shandong Peninsula during the Pleistocene.
中文摘要:
      It has for many years been controversial whether there was a Pleistocene high sea level on the Shandong Peninsula. Our investigations in recent years suggest that the red sandy sediments distributed around the Yuanyaodun village, Weihai County, the "Liukuang Red Bed" and the loess-like deposits near Penglai County should be terrestrial deposits, and there is will not a convincing evidence to confirm that abrasion landforms found above the 10m elevation oa the coast are of marine origin. From these, it is still not safe to say that a high sea level had occurred in the Shandong Peninsula during the Pleistocene.
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