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Jolliff, B.L., Wiseman, S.A., Lawrence, S.J., Tran, T.N., Robinson, M.S., Sato, H., Hawke, B.R., Scholten, F., Oberst, J., Hiesinger, H., van der Bogert, C.H., Greenhagen, B.T., Glotch, T.D. and Paige, D.A. (2011) Non-Mare Silicic Volcanism on the Lunar Farside at Compton-Belkovich. Nature Geoscience, 4, 566-571.
https://doi.org/10.1038/ngeo1212

has been cited by the following article:

• TITLE: Theory of the Origin of Terrestrial and Lunar Ores

  AUTHORS: Alexander N. Safronov

  KEYWORDS: Comet Impact, Galaxy Storm, Galaxy Calm, Elemental Buoyancy Theory, Mantle-Core Layers, Ores Origin

  JOURNAL NAME: International Journal of Geosciences, Vol.14 No.6, June 29, 2023

  ABSTRACT: In this study, the theory of ore formation on the Earth and the Moon was developed. It is shown that ore deposits on the Earth and the Moon were mainly formed simultaneously with the separation of the Moon from the protoplanet and the formation of the oldest continents. The formation of terrestrial ores occurred as a result of the release of intermediate and heavy chemical elements from the deep layers of the protoplanet and the subsequent process of adhesion to old terrestrial geological faults. The time of terrestrial and lunar ores formations corresponds to the boundary between the Tonian and Cryogenian Periods (~720 Ma). Lunar ore formation processes are different on the near and far sides. The farside of the Moon is a single piece of the protoplanetary lithosphere, so ores there could be formed mainly due to the overflow of igneous rocks over the edge of the lunar continent. On the nearside, due to the rapid cooling, ores were formed in the area of navel-string during the drip-liquid separation of the Moon from the Earth. Due to the fact that the Moon separated at the first stage, the amount of water and methane on it is limited. In periods after the Cryogenian, volcanic, lava and sedimentary rocks on Earth could be enriched with intermediate elements due to the disruption of vertical stratification during galactic storms. To analyze this, a comparison of terrestrial volcanic and lunar pseudo-volcanic activity was carried out in the work.