Academic literature on the topic 'Inagli massif'

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Journal articles on the topic "Inagli massif"

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Chaika, I. F., and A. E. Izokh. "Dunites of the Inagli massif (Central Aldan), cumulates of lamproitic magma." Russian Geology and Geophysics 59, no. 11 (November 2018): 1450–60. http://dx.doi.org/10.1016/j.rgg.2018.10.005.

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Rokosova, E. Yu, L. I. Panina, Yu R. Vasil’ev, and F. P. Lesnov. "Conditions of crystallization of olivine shonkinites in the Inagli massif (Central Aldan)." Russian Geology and Geophysics 57, no. 9 (September 2016): 1298–311. http://dx.doi.org/10.1016/j.rgg.2016.08.015.

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Radomskaya, T. A., E. V. Kaneva, R. Yu Shendrik, L. F. Suvorova, and N. V. Vladykin. "Sulfur-Bearing Sodalite, Hackmanite, in Alkaline Pegmatites of the Inagli Massif (Aldan Shield): Crystal Chemistry, Photochromism, and Luminescence." Geology of Ore Deposits 63, no. 7 (December 2021): 696–704. http://dx.doi.org/10.1134/s1075701521070060.

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Zolotarev, Andrey A., Elena S. Zhitova, Faina A. Gabdrakhmanova, Maria G. Krzhizhanovskaya, Anatoly A. Zolotarev, and Sergey V. Krivovichev. "Batisite, Na2BaTi2(Si4O12)O2, from Inagli massif, Aldan, Russia: crystal-structure refinement and high-temperature X-ray diffraction study." Mineralogy and Petrology 111, no. 6 (February 6, 2017): 843–51. http://dx.doi.org/10.1007/s00710-017-0497-z.

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Okrugin, A. V., A. S. Borisenko, A. I. Zhuravlev, and A. V. Travin. "Mineralogical, geochemical, and age characteristics of the rocks of the Inagli dunite-clinopyroxenite-shonkinite massif with platinum-chromite and Cr-diopside mineralization (Aldan Shield)." Russian Geology and Geophysics 59, no. 10 (October 2018): 1301–17. http://dx.doi.org/10.1016/j.rgg.2018.09.008.

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Sokolova, E., F. Cámara, and F. C. Hawthorne. "From structure topology to chemical composition. XI. Titanium silicates: crystal structures of innelite-1T and innelite-2M from the Inagli massif, Yakutia, Russia, and the crystal chemistry of innelite." Mineralogical Magazine 75, no. 4 (August 2011): 2495–518. http://dx.doi.org/10.1180/minmag.2011.075.4.2495.

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AbstractThe crystal structures of two polytypes of innelite, ideally Ba4Ti2Na2M2+Ti(Si2O7)2[(SO4) (PO4)]O2[O(OH)] where M2+ = Mn, Fe2+, Mg, Ca: innelite-1T, a 5.4234(9), b 7.131(1), c 14.785(3) Å, α 98.442(4), β 94.579(3), γ 90.009(4)°, V 563.7(3) Å3, space group P1̄, Dcalc = 4.028 g/cm3, Z = 1; and innelite-2M, a 5.4206(8), b 7.125(1), c 29.314(4) Å, 0 94.698(3)°, V 1128.3(2) Å3, space group P2/c, Dcalc.= 4.024 g/cm3, Z = 2, from the Inagli massif, Yakutia, Russia, have been refined to R values of 8.99 and 7.60%, respectively. Electron-microprobe analysis gave the empirical formula for innelite as (Ba3.94Sr0.06)Σ4.00(Na2.16Mn0.382+Fe2+0.17Mg0.15Ca0.10☐0.04)Σ3(Ti2.97Nb0.02Al0.02)Σ3.01Si4.01 (S1.02P0.81☐0.17)Σ2H1.84O25.79F0.21 which is equivalent to (Ba3.94Sr0.06)Σ4.00(Ti1.97Nb0.02Al0.02)Σ2.01 [(OH0.99F0.21)Σ1.20O0.80], calculated on the basis of 26 (O + F) anions, with H2O calculated from structure refinement. The crystal structure of innelite is a combination of a TS (titanium silicate) block and an I (intermediate) block. The TS block consists of HOH sheets (H-heteropolyhedral, O-octahedral) and exhibits linkage and stereochemistry typical for Ti-disilicate minerals of Group III (Ti = 3 a.p.f.u.): two H sheets connect to the O sheet such that two (Si2O7) groups link to the trans edges of a Ti octahedron of the O sheet. The I block contains T sites, statistically occupied by S and P, and Ba atoms. In the structures of innelite-1T and innelite-2M, TS blocks are related by an inversion centre and a cy glide plane, respectively. HRTEM images show a coherent intergrowth of the two polytypes, together with an as-yet unidentified ∼10 Å phase.
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Tolstykh, Nadezda D. "Platinum mineralization of the Konder and Inagly massifs." Geosfernye issledovaniya, no. 1 (March 1, 2018): 17–32. http://dx.doi.org/10.17223/25421379/6/2.

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"DUNITES OF THE INAGLI MASSIF (Central Aldan), CUMULATES OF LAMPROITIC MAGMA." Геология и геофизика, no. 11 (2018). http://dx.doi.org/10.15372/gig20181105.

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"CONDITIONS OF CRYSTALLIZATION OF OLIVINE SHONKINITES IN THE INAGLI MASSIF (Central Aldan)." Геология и геофизика, 2016. http://dx.doi.org/10.15372/gig20160905.

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"40Ar/39Ar GEOCHRONOLOGY OF ALKALINE ROCKS OF THE INAGLI MASSIF (Aldan Shield, southern Yakutia)." Russian Geology and Geophysics, no. 1 (2019). http://dx.doi.org/10.15372/rgg2019003.

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Dissertations / Theses on the topic "Inagli massif"

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Inagaki, Thiago Massao [Verfasser], Ingrid [Akademischer Betreuer] Kögel-Knabner, Johannes [Gutachter] Lehmann, and Ingrid [Gutachter] Kögel-Knabner. "Organic matter protection through interactions with Fe and Al (hydro) oxides in soil / Thiago Massao Inagaki ; Gutachter: Johannes Lehmann, Ingrid Kögel-Knabner ; Betreuer: Ingrid Kögel-Knabner." München : Universitätsbibliothek der TU München, 2020. http://d-nb.info/1210644150/34.

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Book chapters on the topic "Inagli massif"

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Radomskaya, T. A., N. V. Vladykin, and E. V. Kaneva. "Chemical Compositional Variation of Clinopyroxenes of Alkaline-Ultrabasic and Alkaline Rocks of the Inagli Massif." In Springer Proceedings in Earth and Environmental Sciences, 99–113. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-69670-2_7.

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