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借助于最新的地质、同位素年代学、地球化学和航空地球物理资料,对全球各地原属于罗迪尼亚大陆组成单元的构造环境、地质事件特征及其演化历史进行了探讨,并提出一些新见解和成因模式。认为东欧克拉通在1.7～0.9 Ga 有复杂的演化历史;一个新的劳仑古陆和西伯利亚的重建发生在1 050～1 000 Ma;中、新元古代南美洲造山拼贴的岩石构造历程构成南美陆台的西部边界;非洲克拉通是古元古代/太古宙陆块汇聚收敛的结果;东南极的一部分在中元古时期附属于非洲南部;印度西北的新元古代长英质岩浆事件构成了罗迪尼亚大陆的西部边缘;前格林威尔时期的劳仑古陆已被确定为古元古代末期的一个主要大陆;在罗迪尼亚大陆中,华南可能位于劳仑古陆南部和澳大利亚东部之间;塔里木克拉通和扬子克拉通相连接或邻近。据此检验了关于Pisarevsky提出的罗迪尼亚超大陆汇聚和裂解的新模式。新模式提出初始裂解是沿着劳仑古陆的西部边缘,与大西洋北部相类似。同时认为一些大陆(印度、刚果/圣·弗朗西斯科)可能不是罗迪尼亚超大陆的组成部分。
With the help of the latest geological, isotopic geochronology, geochemistry and aerospace geophysical data, the tectonic environment, geological events and evolution history that belong to the continental units of the Rodinian continents around the world are discussed and some new opinions are put forward And cause pattern. The East European craton is characterized by complex evolutionary history at 1.7-0.9 Ga. The reconstruction of a new Lunlun ancient continent and Siberia occurs at 1,050-1,000 Ma. The rock structure of the Meso-Neoproterozoic South American collage The western boundary of the continental platform in South America; the craton in Africa is the result of convergent convergence of the Paleoproterozoic / Archean terrane; part of the southeast pole is attached to southern Africa in the Middle Proterozoic; the Neoproterozoic marina in Northwestern India The western edge of the mainland of Rodinia; the former Greenland period of Lunlun Palau has been identified as a major ancient Paleocene continental; in the mainland of Rodinia, South China may be located in southern Lunlun and Australia eastern; the Tarim Craton and the Yangtze craton connected or adjacent. Based on this, a new model of the convergence and lysis of the Rodinian continent proposed by Pisarevsky was examined. The new model suggests that the initial lysis is along the western edge of the ancient land of Lunlun, similar to the northern Atlantic. At the same time, it is believed that some of the continents (India, Congo / San Francisco) may not be part of the Rodney supercontinent.