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The Main Types of the Urals Mafic‐Ultramafic Complexes

The Main Types of the Urals Mafic‐Ultramafic Complexes ACTA GEOLOGICA SINICA (English Edition) Vol. 90 Supp. 1 July 2016 http://www.geojournals.cn/dzxben/ch/index.aspx http://mc.manuscriptcentral.com/ags SHMELEV V. R., 2016. The Main Types of the Urals Mafic-Ultramafic Complexes. Acta Geologica Sinica (English Edition), 90(supp. 1): 239-240. SHMELEV V. R. Institute of Geology and Geochemistry, Vonsovsky str. 15, 620016, Ekaterinburg, Russia The mafic-ultramafic complexes and associated induced partial melting with formation of depleted formationsare wide spread within the Ural folded belt, harzburgites (typeIII). In zones of intensive brittle-plastic which is located on the boundary of the East European deformations under the influence of percolating melts and plate and West Siberian sedimentary basin. Two main fluids, the peridotites have experienced types of the complexes having different nature are “depyroxenization” with the formation of dunite bodies distinguished among them– the ophiolite and Ural- and chromite deposits. Alaskan, marking the Main Ural fault (MUF) zone Dunite-clinopyroxenite-gabbro (DCG) complex in the (Savelieva et al., 2002, Efimov, 2010). Urals ophiolite massifs occupies a different position The ophiolite type complexes are well preserved in the relatively the mantle peridotite section. In the normal Polar(Syum-Keu, Rai-Izand Voikar) and South Ural position the dunites, clinopyroxenites (wehrlites) and (Kraka, Habarny, Kempirsay and others) massifs of the layered olivine gabbro are located nearly http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta Geologica Sinica (English Edition) Wiley

The Main Types of the Urals Mafic‐Ultramafic Complexes

SHMELEV, V. R.
Acta Geologica Sinica (English Edition) , Volume 90 (s1) – Oct 1, 2016
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References (8)

Publisher
Wiley
Copyright
© 2016 Geological Society of China
ISSN
1000-9515
eISSN
1755-6724
DOI
10.1111/1755-6724.12996
Publisher site
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Abstract

ACTA GEOLOGICA SINICA (English Edition) Vol. 90 Supp. 1 July 2016 http://www.geojournals.cn/dzxben/ch/index.aspx http://mc.manuscriptcentral.com/ags SHMELEV V. R., 2016. The Main Types of the Urals Mafic-Ultramafic Complexes. Acta Geologica Sinica (English Edition), 90(supp. 1): 239-240. SHMELEV V. R. Institute of Geology and Geochemistry, Vonsovsky str. 15, 620016, Ekaterinburg, Russia The mafic-ultramafic complexes and associated induced partial melting with formation of depleted formationsare wide spread within the Ural folded belt, harzburgites (typeIII). In zones of intensive brittle-plastic which is located on the boundary of the East European deformations under the influence of percolating melts and plate and West Siberian sedimentary basin. Two main fluids, the peridotites have experienced types of the complexes having different nature are “depyroxenization” with the formation of dunite bodies distinguished among them– the ophiolite and Ural- and chromite deposits. Alaskan, marking the Main Ural fault (MUF) zone Dunite-clinopyroxenite-gabbro (DCG) complex in the (Savelieva et al., 2002, Efimov, 2010). Urals ophiolite massifs occupies a different position The ophiolite type complexes are well preserved in the relatively the mantle peridotite section. In the normal Polar(Syum-Keu, Rai-Izand Voikar) and South Ural position the dunites, clinopyroxenites (wehrlites) and (Kraka, Habarny, Kempirsay and others) massifs of the layered olivine gabbro are located nearly

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Acta Geologica Sinica (English Edition) – Wiley

Published: Oct 1, 2016

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