中国东部晚震旦—早寒武世含磷建造分析和聚磷沉积模式
ANALYSIS OF PHOSPHATIC FORMATlON AND SEDIMENTARY MODEL OF PHOSPHATIC ACCUMULATl0N OF UPPER SINIAN-LOWER CAMBRIAN SYSYTEM IN CHINA
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摘要: 含磷建造系指含有磷块岩的沉积建造。中国东部晚震旦—下寒武世发育有分布广泛而又有工业意义的含磷建造带。深入研究这一时期的含磷建造对阐明古老磷块岩形成机理和大地构造背景,以及磷矿远景预测工作都具有重要意义。Abstract: According to the threefold meaning of rock一paragenesis suggested by the author and based on the material source ,environment and energy- equilibrium，the phosphatie formation in the eastern part of China 560-700 Ma has been div-ided into mono-terrestrial formation.tele-siliceous formation and silice ous shale formation ,all belonging to stable type，substable type and unstable type forma-lions, respectiveli.
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(2) 孟祥化，(1979)远硅质建造磷块岩微相研究，地球化学，第2期，第I32-144页。
(3) r. u.布中斯基、叶连俊、郑直，(1959)中国磷矿形成分布的规律及今后需要研究的问题，中国磷块岩的形成特点矿石类型及远景评价，科学出版社。
(4) Valloni，R.&Mapnard,J.B.，(1981)Detrital Modes of Recent Deep Sea Sands and Their Relation to Tectonic Setting; A First Approximation，SedimentoloEv，V.28,N.1 75-83。 -
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