ADVANCES IN STUDY OF CHINA’S SHELF QUATERNARY GEOLOGY
Received date: 1994-11-17
Online published: 1995-12-01
于洪军,刘敬圃 . 中国陆架第四纪地质学研究的最新进展[J]. 地球科学进展, 1995 , 10(6) : 531 -536 . DOI: 10.11867/j.issn.1001-8166.1995.06.0531
From the1950’s, the study of China’s continental shelf Geology has made great progress, especially in the study of the environmental evolution of Late Quaternary. This paper summarized the new advances in this field.
1.Environmental evolution on the China’s shelf during the LGM period:
①Sea-level changes and land-ocean distribution during the LGM period;
②The prevailed winter monsoon and its environmental effect;
③Relationship of sea-level and river retreated and extended.
2.The shelf desertization and its evidences during the LGM period in the marine stratum:
①Cold-dry environment extended into the exposed shelf region;
②Aeolian deposits and derivative sediment on the shelf;
③Buried geomorphological evidences of shelf desertization.
3.Origin of the buried loess in the sea bottom and exposed loess in the coastal zone:
①The relationship of desert and loess deposits;
②Shelf desertization and the coastal loess;
③The strong paleomonsoon prevailed and loess accumulation on the exposed shelf area.
[1] Eery K O. Continental shelf sediments of southern of southern California. Bull Geol Soc Amer,1952,63:1105-1110.
[2] 郑光膺. 南黄海第四纪层型地层对比.北京:科学出版社,1989.1-275.
[3] 安芷生,吴锡浩,汪品先等.末次间冰期以来中国古季风气候与环境变迁.黄土•第四纪地质•全球变化(三),刘东生,安芷生主编.北京:科学出版社,1992.14-30.
[4] CLIMAP Project Members. The surface of the ice age earth.Science,1976,191:1131-1137.
[5] 赵松龄.苏北浅滩成因的最新研究.海洋地质与第四纪地质,1991,11(3):1105-1126.
[6] 赵松龄,于洪军.陆架沉积环境研究的若干新进展.中国沙漠,1993,13(4):1-5.
[7] Prospero J M. Eolian transport to the world ocean. THESEA,7 A Willy-Interscience Publication,1981.801-874.
[8] Bowles J M.Aridity in Australia: age,origins and expression in Aeolian landforms and sediments. Earth Sci Rev,1976,12:279-310.
[9] An Zhisheng et al. East Asian Winter Monsoon Variation associated with Global Ice Volume Cycle and Accumulation of Chinese Loess. Abstract Collection: International Symposium on Global Change in Asia and the Pacific Regions,1994.1-1.
[10] 赵松龄.晚更新世末期中国陆架沙漠化及其衍生沉积.海洋与湖沼,1991,22(3):285-293.
[11] Flint R F. Glacial Geology and the Pleisticene Epoch.1955,175-187.
[12] Pye K. Aeolian Dust and Dust Deposits. Academic Press.1987,68pp.
[13] Zarate M,Blasi A.Late Pleistocene-Holocene Eolian Deposits of the Southern Buenos Airs Province,Argentina: Apreliminary model,Quternary International. 1993,17:15-20.
[14] 董光荣.晚更新世以来我国北方沙漠地区的气候变化.第四纪研究.1990,3:214-222.
[15] 刘东生.黄土与环境.北京:科学出版社,1985.207•
[16] Zhao Songling and Li Guogang. Desertization on the sheves adjacent China in the later late Pleistocene. Oceanologia et Limnologia Sinica,1990,8(4):289-298.
[17] 曹家欣,李培英,石宁.山东庙岛群岛的黄土.中国科学B辑,1987,17:1116-1123.
[18] 李培英等.辽东海岸带黄土.地质学报,1992,66(2):82-93.
[19] Liu Jingpu,Yu Hongjun. The origin of the loess along the Bohai sea coastal zone,Abstract Collection: International Symposiumon Global Change in Asia and the Pacific Regions,1994.1-4.
/
〈 |
|
〉 |