摘要
The two phosphatic formations distributed in Yunan-Guizhon-Sichuan(Lower Cambrian)and Hubci-Hunan-Guizhou(Late Sinian)which were originally thought to be terrestrial carbonate deposits should be regarded as tele-siloceous formation in character as is evidenced by regional formation sequence patterns. The implications of this observation arc discussed with respect to tectonic and prospecting for P,I, and other base metals. In the light of detailed investigation on mierophase composition microphase Zoning and those features concerning depositional environment and geochemistry a mechanism of phosphate accumulation is proposed with special reference to the role of dynamic chemistry, F, palaeotectonics and palaeoelimatology. It is pointed out by the author that the proposal of chemical deposition suggested by A. V.Kazakov is in conflict with the model of microphase zonation and formation sequence patterns. The relationship is also dealt with between the ratios of CO2/P2O5 and F/P2O5 on the one hand and the mechanism of phosphate accumulation on the other.
The two phosphatie formations distributed in Yunan-Guizhou-Sichuan (Lower Cambrian) and Hubei-Hunan-Guizhou (Late Sinian) which were originally thought to be terrestrial carbonate deposits should be regarded as tele-siliceous formation in character as is evidenced by regional formation sequence patterns.The implications of this observation are discussed with respect to tectonic and prospecting for P,I,and other base metals.In the light of detailed investigation on microphase composition microphase Zoning and those features concerning depositional environment and geochemistry,a mechanism of phosphate accumulation is proposed with special reference to the role of dynamic chemistry,F,palaeotectonics and palaeoclimatology.It is pointed out by the author that the proposal of chemical deposition suggested by A.V.Kazakov is in conflict with the model of microphase zonation and formation sequence patterns.The relationship is also dealt with between the ratios of CO2/P2O5 and P/P2O5 on the one hand and the mechanism of phosphate accumulation on the other.
出处
《地球化学》
CAS
1979年第2期132-144,i010,共14页
Geochimica
