The article describes the mineral composition and petrochemistry of a unique ancient (more than 1848–2011 MA) igneous rock of the Urals – plagioclase olivine clinopyroxenite. These rocks are considered the oldest in the Urals. In the literature they are described under the name izrandites. They are part of the foundation of the basement of the East European platform. These rocks are highly aluminous and calcic. They are characterized by a low amount of alkalis and magnesium oxide and a comparable amount of silicon and iron. A certain petrochemical similarity is found between the izrandites and the anorthite leucogabbro, troctolite, and noritic anorthosites of lunar highlands. This similarity enhances the closeness of distribution of the minor elements, the leading role among which belongs to Sr and Ba. In those and others rocks plagioclase is represented by anorthite or labrador, its amount makes up from 5–8 to 50–70%. The izrandites are representatives of the rocks of the lower part of the Earth's crust, which in composition and absolute age can be compared with the youngest leucogabbros and troctolites of the Moon.
| Published in | Earth Sciences (Volume 8, Issue 2) |
| DOI | 10.11648/j.earth.20190802.13 |
| Page(s) | 94-101 |
| Creative Commons |
This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited. |
| Copyright |
Copyright © The Author(s), 2019. Published by Science Publishing Group |
Olivine Clinopyroxenite, Izrandite, Anorthosite, Leucogabbro, Urals, Earth, Moon
| [1] | Anfilogov VN, Khatchay YV, Antipin AN (2015) About relationship of the compositions of matter of the Moon, primary Earth crust and mantle. Lithosphere 1: 109–115 (in Russian). |
| [2] | Apollo 17. Mission report (1973) Lyndon B. Johnson center, Houston. Texas. |
| [3] | Barsukov VL, Dmitriev LV, Garanin AV (1979) Basic features of geochemistry of Lunar rocks. In: Ground from continental area of the Moon. Nauka, Мoskow, pp 18–30 (in Russian). |
| [4] | Bogatikov OA, Gon’shakova VI, Frikh–Khar DI. (1983) Classification of lunar igneous rocks and their comparison with terrestrial analogues. In: Sharkov EV (ed.), Magmatic rocks III. Nauka, Мoscow, pp 395–402 (in Russian). |
| [5] | Borg LE, Connely JN, Boyet M, Carlson RW (2011) Chronological evidence that the Moon is either young or did not have a global magma oceprobe Nature 477 (7362): 70–72. |
| [6] | Delano JW (2009) Scientific exploration of the Moon. Elements 5: 11–16. |
| [7] | Frondel JW (1975) Lunar mineralogy. Wiley, New York, London. |
| [8] | Hammarström JM, Zen E–An (1986) Aluminium in hornblende: an empirical igneous geobarometer. Am Miner 71: 1297–1313. |
| [9] | Haskin LA, Helmke HA, Blanchard DP, Jacobs JW, Telander K (1973) Major and trace elements abundaces in samples from the lunar highlands. In Proceedings of the Fourth Lunar Science Conferens (Supplement 4). Geochim Cosmochim Acta 2: 1275–1296. |
| [10] | Hui HJ, Peslier AH, Zhang Y, Neal CR (2013) Water in lunar anorthosites and evidence for a wet early moon. Nature Geosci 6: 177–180. |
| [11] | Ivanov OK (1997) Concentric–zonal pyroxenite–dunite massifs of the Urals. Urals University Publ, Ekaterinburg (in Russian). |
| [12] | Jolliff BL, Wieczorek MA, Shearer CK, Neal CR (2006) New Views of the Moon. Rev Mineral Geochem 60. |
| [13] | Korinevsky VG, Korinevsky EV (2006) The new in geology, petrography and mineralogy of the Il’meny Mountains. IMIN UB RAS, Miass (in Russian). |
| [14] | Korinevsky VG, Kotlyarov VA (2009) Mineralogy of plagioclase-olivine clinopyroxenite (izrandite) of the Urals. Lithosphere 4: 27–40 (in Russian). |
| [15] | Krasnobaev AA, Cherednichenko SV (2004) Zircon geochronology of the Alexandrovskiy metamorphic complex (South Urals). Doklady of RAS 396 (4): 519–523 (in Russian). |
| [16] | Lennykh VI, Valizer PM (2006) To the geological scheme of the Il’menogorskiy complex. In: Geology and mineralogy of the Il’menogorskiy complex: situation and problems. Il’menian Reserve Publ, Miass, pp 20–27 (in Russian). |
| [17] | Loucks RR (1996) A precise olivine–augite Mg – Fe exchange geothermometer. Contrib Mineral Petrol 125 (2–3): 140–150. |
| [18] | Nazarov MA, Tarasov LS, Shevaleevsky ID (1979) Mineralogy of mainland regolith (“Moon–20”). In: Ground from continental area of the Moon. Nauka, Мoscow, pp 226–266 (in Russian). |
| [19] | Neal CR (2009) The Moon 35 years after Apollo: What’s left to learn? Chemie der Erde 69: 3–43. |
| [20] | Norman MD, Borg LE, Nyquist LE, Bogard DD (2003) Chronology, geochemistry, and petrology of a ferroan noritic anorthosite clast from Descartes breccia 67215: clues to the age, origin, structure, and impact history of the lunar crust. Meteor Planet Sci 38 (4): 645–661. |
| [21] | O'Hara MJ, Niu YL (2015) Obvious problems in lunar petrogenesis and new perspectives. In: The interdisciplinary earth: a volume in honor of Don l. Anderson. Boulder, Colorado: The Geological Society of America, the American Geophysical Union, pp 339–366. |
| [22] | Ovchinnikov LN Dunaev VA (1968) About geological oldest deep rock of the Urals. In: Deep structure of the Urals. Nauka, Moscow, pp 200–209 (in Russian). |
| [23] | Pystin AM (1978) Aleksandrovskiy gneiss-amphibolite complex. In: Volcanism, metamorphism and ferruginous quartzites of the Taratash complex. UNTs of the USSR Academy of Sciences, Sverdlovsk, pp 3–32 (in Russian). |
| [24] | Pystin AM, Pystina SN, Lennykh VI (1973) About geological setting of izrandites in the Alexandrovskiy complex (western slope of the Urals). In: Ezhegodnik–1972 of the IGG UB RAS, Sverdlovsk, pp 96–97 (in Russian). |
| [25] | Ronkin YuL, Sindern S, Kramm U, Lepikhina OP (2008) Isotopic geology of the earliest formations of the Urals: U-Pb, Sm-Nd, Rb-Sr and 40Ar-39Ar systematics. In: Structural-real complexes and problems of geodynamics Precambrian of the Phanerozoic orogens. UB RAS, Ekaterinburg, pp 117–120. |
| [26] | Saal AE, Hauri EH, Lo Cascio M, Van Orman JA, Rutherford MC, Cooper RF (2008) Volatile content of lunar volcanic glasses and the presence of water in the Moon’s interior. Nature 454: 192–195. |
| [27] | Sharkov EV, Bogatikov OA (1983) Layered intrusions of basic and ultrabasic rocks. In: Sharkov EV (ed.), Magmatic rocks III. Nauka, Мoscow, pp 72–103 (in Russian). |
| [28] | Sharkov EV, Krasivskaya IS, Chistyakov AV (2004) Dispergeric mafite–ultramafite intrusive magmatism of the Early–Paleoproterozoic mobil zones of the Baltic shield: e.g. druzite (coronite) complex of the Belomoriya. Petrology 12 (6): 632–655 (in Russian). |
| [29] | Smith JV (1980) Was a hydrous and carbonated magma present on the Moon? Lunar Planet Sci XII: 1005–1007. |
| [30] | Tomilenko AA, Kovyazin SV (2008) Formation of the coronite structures around olivine in the Korosten pluton anorthosites, Ukranian shield: mineralogy, geochemistry, fluid inclusions. Petrology 16 (1): 92–109 (in Russian). |
| [31] | Wager LP, Brown GM (1968) Layered igneous rocks. Oliver & Boyd, Edinburg, London. |
| [32] | Watters TR., Robinson M, Beyer RA, Banks ME, Bell J, Pritchard ME, Williams NR (2010). Evidence of recent thrust faulting on the moon revealed by the lunar reconnaissance orbiter camera. Science 329 (5994): 936–940. |
| [33] | Whitney DL, Evans BW (2010) Abbreviations for names of rock–forming minerals. Am Mineral 95: 185–187. |
| [34] | Yaroshevsky AA (1979) Zonal melting of the Lunar crust rocks. In: Ground from continental area of the Moon. Nauka, Мoscow, pp 327–335 (in Russian). |
APA Style
Victor Grigorievich Korinevsky, Eugeny Victorovich Korinevsky. (2019). Terrestrial Plagioclase Olivine Clinopyroxenite as a Possible Analogue of Lunar Rocks. Earth Sciences, 8(2), 94-101. https://doi.org/10.11648/j.earth.20190802.13
ACS Style
Victor Grigorievich Korinevsky; Eugeny Victorovich Korinevsky. Terrestrial Plagioclase Olivine Clinopyroxenite as a Possible Analogue of Lunar Rocks. Earth Sci. 2019, 8(2), 94-101. doi: 10.11648/j.earth.20190802.13
AMA Style
Victor Grigorievich Korinevsky, Eugeny Victorovich Korinevsky. Terrestrial Plagioclase Olivine Clinopyroxenite as a Possible Analogue of Lunar Rocks. Earth Sci. 2019;8(2):94-101. doi: 10.11648/j.earth.20190802.13
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Download@article{10.11648/j.earth.20190802.13,
author = {Victor Grigorievich Korinevsky and Eugeny Victorovich Korinevsky},
title = {Terrestrial Plagioclase Olivine Clinopyroxenite as a Possible Analogue of Lunar Rocks},
journal = {Earth Sciences},
volume = {8},
number = {2},
pages = {94-101},
doi = {10.11648/j.earth.20190802.13},
url = {https://doi.org/10.11648/j.earth.20190802.13},
eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20190802.13},
abstract = {The article describes the mineral composition and petrochemistry of a unique ancient (more than 1848–2011 MA) igneous rock of the Urals – plagioclase olivine clinopyroxenite. These rocks are considered the oldest in the Urals. In the literature they are described under the name izrandites. They are part of the foundation of the basement of the East European platform. These rocks are highly aluminous and calcic. They are characterized by a low amount of alkalis and magnesium oxide and a comparable amount of silicon and iron. A certain petrochemical similarity is found between the izrandites and the anorthite leucogabbro, troctolite, and noritic anorthosites of lunar highlands. This similarity enhances the closeness of distribution of the minor elements, the leading role among which belongs to Sr and Ba. In those and others rocks plagioclase is represented by anorthite or labrador, its amount makes up from 5–8 to 50–70%. The izrandites are representatives of the rocks of the lower part of the Earth's crust, which in composition and absolute age can be compared with the youngest leucogabbros and troctolites of the Moon.},
year = {2019}
}
TY - JOUR T1 - Terrestrial Plagioclase Olivine Clinopyroxenite as a Possible Analogue of Lunar Rocks AU - Victor Grigorievich Korinevsky AU - Eugeny Victorovich Korinevsky Y1 - 2019/04/29 PY - 2019 N1 - https://doi.org/10.11648/j.earth.20190802.13 DO - 10.11648/j.earth.20190802.13 T2 - Earth Sciences JF - Earth Sciences JO - Earth Sciences SP - 94 EP - 101 PB - Science Publishing Group SN - 2328-5982 UR - https://doi.org/10.11648/j.earth.20190802.13 AB - The article describes the mineral composition and petrochemistry of a unique ancient (more than 1848–2011 MA) igneous rock of the Urals – plagioclase olivine clinopyroxenite. These rocks are considered the oldest in the Urals. In the literature they are described under the name izrandites. They are part of the foundation of the basement of the East European platform. These rocks are highly aluminous and calcic. They are characterized by a low amount of alkalis and magnesium oxide and a comparable amount of silicon and iron. A certain petrochemical similarity is found between the izrandites and the anorthite leucogabbro, troctolite, and noritic anorthosites of lunar highlands. This similarity enhances the closeness of distribution of the minor elements, the leading role among which belongs to Sr and Ba. In those and others rocks plagioclase is represented by anorthite or labrador, its amount makes up from 5–8 to 50–70%. The izrandites are representatives of the rocks of the lower part of the Earth's crust, which in composition and absolute age can be compared with the youngest leucogabbros and troctolites of the Moon. VL - 8 IS - 2 ER -
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