The obtained evidence of hot heterogeneous accretion of the Earth leads to a fundamentally new solution to genetic problems. According to these data, the kimberlites were formed as a result of the rise of the last residual melts of the bottom peridotite layer of the magmatic ocean, which arose as a result of impact heat release during accretion. The diamond crystallized due to the accumulation of carbon in the residual melts during fractionation. The absence of kimberlites in oceanic and collision regions is due to the expansion of the fractionation products of the magmatic ocean by surfaced mantle plumes during the formation of these regions. The all-earth distribution of the magmatic ocean explains the presence of kimberlites on all the studied ancient platforms. A very high degree of crystallization of the peridotite layer is the reason for the small volume of kimberlite residual melts and the bodies formed by them. The low temperature of kimberlite magmas caused their decompression solidification after boiling at the shallow stage of ascent and explosion under the influence of the high pressure of the fluid phase preserved by solidification. This is the reason for the formation of kimberlite pipes and the absence of kimberlite lavas.
Published in | Earth Sciences (Volume 10, Issue 4) |
DOI | 10.11648/j.earth.20211004.12 |
Page(s) | 157-164 |
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Kimberlites, Diamond, Magmatic Ocean, Decompression Solidification
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APA Style
Vladimir Shkodzinsky. (2021). Nature of the Features of Kimberlite Placement. Earth Sciences, 10(4), 157-164. https://doi.org/10.11648/j.earth.20211004.12
ACS Style
Vladimir Shkodzinsky. Nature of the Features of Kimberlite Placement. Earth Sci. 2021, 10(4), 157-164. doi: 10.11648/j.earth.20211004.12
AMA Style
Vladimir Shkodzinsky. Nature of the Features of Kimberlite Placement. Earth Sci. 2021;10(4):157-164. doi: 10.11648/j.earth.20211004.12
@article{10.11648/j.earth.20211004.12, author = {Vladimir Shkodzinsky}, title = {Nature of the Features of Kimberlite Placement}, journal = {Earth Sciences}, volume = {10}, number = {4}, pages = {157-164}, doi = {10.11648/j.earth.20211004.12}, url = {https://doi.org/10.11648/j.earth.20211004.12}, eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20211004.12}, abstract = {The obtained evidence of hot heterogeneous accretion of the Earth leads to a fundamentally new solution to genetic problems. According to these data, the kimberlites were formed as a result of the rise of the last residual melts of the bottom peridotite layer of the magmatic ocean, which arose as a result of impact heat release during accretion. The diamond crystallized due to the accumulation of carbon in the residual melts during fractionation. The absence of kimberlites in oceanic and collision regions is due to the expansion of the fractionation products of the magmatic ocean by surfaced mantle plumes during the formation of these regions. The all-earth distribution of the magmatic ocean explains the presence of kimberlites on all the studied ancient platforms. A very high degree of crystallization of the peridotite layer is the reason for the small volume of kimberlite residual melts and the bodies formed by them. The low temperature of kimberlite magmas caused their decompression solidification after boiling at the shallow stage of ascent and explosion under the influence of the high pressure of the fluid phase preserved by solidification. This is the reason for the formation of kimberlite pipes and the absence of kimberlite lavas.}, year = {2021} }
TY - JOUR T1 - Nature of the Features of Kimberlite Placement AU - Vladimir Shkodzinsky Y1 - 2021/08/18 PY - 2021 N1 - https://doi.org/10.11648/j.earth.20211004.12 DO - 10.11648/j.earth.20211004.12 T2 - Earth Sciences JF - Earth Sciences JO - Earth Sciences SP - 157 EP - 164 PB - Science Publishing Group SN - 2328-5982 UR - https://doi.org/10.11648/j.earth.20211004.12 AB - The obtained evidence of hot heterogeneous accretion of the Earth leads to a fundamentally new solution to genetic problems. According to these data, the kimberlites were formed as a result of the rise of the last residual melts of the bottom peridotite layer of the magmatic ocean, which arose as a result of impact heat release during accretion. The diamond crystallized due to the accumulation of carbon in the residual melts during fractionation. The absence of kimberlites in oceanic and collision regions is due to the expansion of the fractionation products of the magmatic ocean by surfaced mantle plumes during the formation of these regions. The all-earth distribution of the magmatic ocean explains the presence of kimberlites on all the studied ancient platforms. A very high degree of crystallization of the peridotite layer is the reason for the small volume of kimberlite residual melts and the bodies formed by them. The low temperature of kimberlite magmas caused their decompression solidification after boiling at the shallow stage of ascent and explosion under the influence of the high pressure of the fluid phase preserved by solidification. This is the reason for the formation of kimberlite pipes and the absence of kimberlite lavas. VL - 10 IS - 4 ER -