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大陆地块的沉积地球化学苏联科学院从1930年起,就已开始对它进行研究。阿尔汉格尔斯基、罗日科娃.斯特拉霍夫等曾对P、V、Cu在明显富含有机质的沉积岩层形成过程中的性状作了估计。最初,这一问题是以现代黑海沉积物为例进行研究的,此后,对受到十分强烈的成岩改造的古老沥青页岩进行了研究。阿尔汉格尔斯基和科普切诺娃的著作对不同地球化学环境中形成的不同类型的铁矿石的化学成分作了描述。为此目的,作者测定了200个样品中的P、As、Mn、V、Cr、
Sedimentary geochemistry of the mainland plots The Soviet Academy of Sciences has been studying it since 1930. Arkhangelski, Rozhkova. Strahov et al. Have estimated the traits of P, V, Cu in the formation of clearly organic-rich sedimentary rocks. Originally, this issue was studied in the case of the modern Black Sea sediments, after which time ancient bitumen shales that had undergone very strong diagenetic modifications were studied. The writings of Arkhangelski and Copchinova describe the chemical composition of different types of iron ores formed in different geochemical environments. For this purpose, the authors measured the P, As, Mn, V, Cr,