5,10,15,20-Tetrakis (p-4-fluorobenzoyloxy) phenyl Porphyrin and Its Transition Metal Complexes

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<正> 近年来,对碳酸盐岩沉积环境的分析已广泛展开,尤其在古生代及其以后的碳酸盐岩中相继建立了不少标准型沉积环境(相)模式,但对前寒武纪碳酸盐岩沉积环境(相)的研究则较少