Probe into the origin, development and evolution model of shelf desertizational environment in the last stage of Late Pleistocene[J]. 海洋湖沼学报(英文), 1998,16(4):326-332.
Hong-jun, Y., Jing-pu, L. & Qiu-mei, S. Probe into the origin, development and evolution model of shelf desertizational environment in the last stage of Late Pleistocene., Chin. J. Ocean. Limnol. 16, 326–332 (1998). https://doi.org/10.1007/BF02844929
Probe into the origin, development and evolution model of shelf desertizational environment in the last stage of Late Pleistocene[J]. 海洋湖沼学报(英文), 1998,16(4):326-332. DOI: 10.1007/BF02844929.
Hong-jun, Y., Jing-pu, L. & Qiu-mei, S. Probe into the origin, development and evolution model of shelf desertizational environment in the last stage of Late Pleistocene., Chin. J. Ocean. Limnol. 16, 326–332 (1998). https://doi.org/10.1007/BF02844929DOI:
Probe into the origin, development and evolution model of shelf desertizational environment in the last stage of Late Pleistocene
摘要
Abstract
Based on study of China's shelf paleoenvironment
this paper summarises the definition of shelf desertization that occurred in the last stage of Late Pleistocene
and discusses the background of its formation and evolution process. Study of shallow layer profiler records and core data revealed that cold-dry aeolian erosion was the major exogenic force on the exposed shelf. Under the prevailing paleo-winter monsoon
part of the exposed marine stratum disintegrated into sand and then desertization occurred. The fine sediments were blown away and deposited on the leeward to form derivative loess deposits.
关键词
Keywords
references
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