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CARBONATE EOLIANITES IN PUTIAN,FUJIAN (Ⅱ)——SEDIMENTATION AND DIAGENESIS
引用本文:赵希涛,沙庆安,李平日,王绍鸿,韩有松,张秀荣,张德泉.CARBONATE EOLIANITES IN PUTIAN,FUJIAN (Ⅱ)——SEDIMENTATION AND DIAGENESIS[J].中国科学B辑(英文版),1990(10).
作者姓名:赵希涛  沙庆安  李平日  王绍鸿  韩有松  张秀荣  张德泉
作者单位:Institute of Geology,Academia Sinica,Beijing 100029,PRC,Institute of Geology,Academia Sinica,Beijing 100029,PRC,Guangzhou Institute of Geography,Guangzhou 510070,PRC,Institute of Geography,Fujian Teachers University,Fuzhou 350007,PRC,Institute of Oceanography,Academia Siniea,Qingdao 266071,PRC,Institute of Oceanography,Academia Siniea,Qingdao 266071,PRC,Teachers College of Putian,Putian 351100,PRC
基金项目:Project supported by both the National Natural Science Foundation of China and Academia Sinica.
摘    要:On the basis of Ref. 1] entitled "Carbonate eolianites in Putian, Fujian (Ⅰ)——Sedimentary structures and paleowinds", the sediment composition, sedimentary textures and diagenesis of the quartz-calcarenites in Houshijing, Putian, Fujian are described here and compared with those of adjacent modern dune and beach sands, and their genesis and sources of sediment are discussed further. The authors consider that they are carbonate eolianites which were formed by coastal dune sand derived from reworking of adjacent beach sand by prevailing northeast monsoon winds and then cemented by freshwater subaerially during the end of the Middle Holocene.

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