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《Acta Sedimentologica Sinica》 1983-02
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ANALYSIS OF PHOSPHATIC FORMATION AND SEDIMENTARY MODEL OF PHOSPHATIC ACCUMULATION OF UPPER SINIAN-LOWER CAMBRIAN SYSTEM IN CHINA

Meng Xianghua ( Changchun College of Geology )  
According to the threefold meaning of rock-paragenesis suggested by the author and based on the material source .environment and energy equilibrium, the phosphatic formation in the eastern part of China 560-700 Ma has been divided into mono-terrestrial formation, tele-siliceous formation and silice ous shale formation,all belonging to stable type, substable type and unstable type formations, respectively. The giant phosphorus-rich accumulation zone belonging to the characteristic of tele-siliceous formation possesses the combined model of CF+SF+MF+OF with lower value Q ( 49% ).In the phosphate-rich constituent Na is higher than K,with lower TiO_2,and Al_2O_3.In respect to the relationship between the alternating sequence of sedimentary formations and the spatial distribution,it belongs to the component part of the volcanic-siliceous formation and possesses the characteristics of marginal basin connected with back arc basin.The sources of the elements P, F, I, V,Ni,Mo,Co,Cu ,U and Y are related to the oceanic volcanic action. The phosphorus-rich accumulation zone of tele-siliceous formation includes four models; chemical deposition ( M-Ⅰ ),algal deposition ( M-Ⅱ ) ,hydrodynamic deposition ( M-Ⅲ ) and gravity gliding superimposition ( M-Ⅳ ) . The writer has analysed the special conditions of tectonics and paleogeog-raphy for the formation of phosphorus-rich deposit by using paleogeographic mapping, comparative sedimentology and comparative sedimentary formational, geology.The paleogeographic settings are the margins of small-scale land-mass, insufficient import of terrigenous fragments and the characteristics of clean-water basin. And the sedimentary framework is that the deep-water depression alternates with shallow-sea platform under the effect of the back are basin. The depressions between platforms are favourable for the import of phosphorus-rich materials from the deep sea, and the clean shallow-sea platform is favourable for the phosphorus accumulations of chemical, algal and hydrodynamic depositions. The gravity gliding superimposition can only occur in the said sedimentary formation.
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