Preview

Литосфера

Расширенный поиск

Ancient age of zircons and issues associated with the genesis of dunites from gabbro-ultrabasite complexes of orogenic areas and central-type platform massifs

Аннотация

The determination of ancient ages of zircons in dunites from the orogenic regions and central-type platform massifs raised a number of issues: 1) the equilibrium of zircon with dunite material and, as a result, the possibility of determining the age of dunite using zircon; 2) polychronic zircons in dunites and the mechanism for the formation of zoned zircon crystals; 3) the origin of the oldest dunite material dated at more than 2500 Ma; 4) mechanism for the formation of zoned zircon crystals in dunite. The article presents results of studying phase equilibrium in the system MgO–SiO2–ZrO2, which confirmed the possibility of zircon crystallisation in equilibrium with olivine and pyroxene. It was found that zircon is stable in dunite up to 1450°C, whereas at higher temperatures zircon is replaced by baddeleyite. It is shown that zoned zircon crystals can be formed in dunite as a result of the gradual transformation of zircon into baddeleyite and vice versa. Drawing on the experimental data, the authors proposed a mechanism for the accumulation of dunite material in the form of restite, which forms during the partial melting of mantle peridotite, as well as the possible way for dunite resitite to raise to the surface in the form of diapir. The difference between the Ural alpine-type ultrabasites and the ultrabasites of the Platiniferous Belt is discussed. It is proposed that the alpine-type ultrabasite occur сloser to the surface where they actively interact with water.

Ключевые слова


Об авторах

V. N. Anfilogov
Institute of Mineralogy, Ural Branch of RAS
Россия

Vsevolod N. Anfilogov

Ilmeny Reserve, Miass, 456317



A. A. Krasnobaev
Zavaritsky Institute of Geology and Geochemistry, UB RAS
Россия

Artur A. Krasnobaev

15 Akad. Vonsovsky St., Ekaterinburg, 620016



V. M. Ryzhkov
Institute of Mineralogy, Ural Branch of RAS
Россия

Vyacheslav M. Ryzhkov

Ilmeny Reserve, Miass, 456317



Список литературы

1. Anfilogov V.N. (2010) Origin of andesite and rhyolite of complementary magma series. litosfera, (1), 37-46. (In Russian)

2. Anfilogov V.N., Khachai Yu.V. (2000) Hydroextrusion is a possible mechanism for the movement of diapirs, domes and mantle plumes. Geokhimiya, (8), 873-878. (In Russian)

3. Anfilogov V.N., Khachai Yu.V. (2007) Superplumes: tectonics, magmatism, metamorphism. “Geodinamika formirovaniya podvizhnykh pojasov zemli”. materialy mezhdunar. konferentsii [“Geodynamics of the formation of mobile belts of the earth”. materials of the Intern. conf.]. Ekaterinburg, IGG, UB of RAS, 6-9. (In Russian)

4. Anfilogov V.N., Krasnobaev A.A., Ryzhkov V.M., Valizer P.M. (2017) Replacement of zircon with baddeleyite as a likely mechanism of the formation of zoned zircon crystals in ultrabasic rocks. Dokl. Earth sci., 475(2), 946-948.

5. Anfilogov V.N., Purtov V.K. (1976) Mechanism of interaction of pore solutions with magmatic bodies. Geokhimiya, (9), 1400-1403. (In Russian)

6. Anfilogov V.N., Ryzhkov V.M., Blinov I.A., Krasnobaev A.A., Kabanova L.Y., Valizer P.M. (2015) Stability of zircon in dunite at 1400–1550°C. Dokl. Earth sci., 464(1), 963-966.

7. Anikina E.V., Krasnobaev A.A., Rusin A.I., Busharina S.V., Kapitonov I.N., Lokhov K.I. (2012) Isotope-geochemical characteristics of zircon from dunites, clinopyroxenites and gabbro Platinum belt of the Urals. Dokl. akad. Nauk, 443(6), 711-715. (In Russian)

8. Bea F., Fershtater G.B., Montero P., Whitehous M., Le vin V.Ya., Scarrow J.H., Austrheim H., Pushkariev E.V. (2001) Recicling of continental crust into mantle as revealed by Kytlym dunite zircons, Ural. Terra Nova, 13(6), 407-412.

9. Bortnikov N.S., Sharkov E.V., Bogatikov O.A., Zinger T.F., Lepekhina E.N., Antonov A.V., Sergeev S.A. (2008) Finds of young and ancient zircons in gabbroids of the Markov deep, mid-atlantic ridge, 5°54′-5°02.2′ N (results of SHRIMP-II U-PB dating): implication for deep geodynamics of modern oceans. Dokl. Earth sci., 421(1), 859-866.

10. Burg J.P., Bodiner J.L., Gerya T., Bedini R.M., Boudier F., Daurtria J.M., Prikhodko V., Efimov A., Pupier E., Balanec J.L. (2009) Translithospheric mantle diapirism. Geological evidence and numerical modeling of the Kondyor ultramafic complex (Russian Far-East). J. petrol., 50(2), 289-321.

11. Сarter N.L., Ave’Lallement H.G. (1970) High temperature flow of dunite and periditite. Geol. soc. amer. Bull., 81, 2181-2202.

12. Chashchukhin I.S., Votyakov S.L, Shchapova Yu.V. (2007) Kristallokhimiya khromshpineli i oksitermobarometriya ul’tramafitov skladchatykh oblastei [Crystallochemistry of chrome spinels and oximetromobarometry of ultramafites of folded regions]. Ekaterinburg, 310 p. (In Russian)

13. Corfu F., Hanchar J.M., Hoskin p.W.O., Kinny p. (2003) atlas of zircon texture. Rev. Mineral. Geochim., 53, 469-500.

14. Davidson A., van Breemen O. (1998) Baddeleite-zircon relationship in coronic metagabbro, greville province, Ontario: implication for geochronology. contrib. Mineral. petrol., 100, 291-299.

15. Efimov A.A. (1995) High-temperature aqueous metamorphism in the Рlatiniferous Belt of the Urals: Tectonic regime and metamorphic reactions. aktual’nye problemy magmaticheskoi geologii, petrologii i rudoobrazovaniya [Actual problems of magmatic geology, petrology and ore formation]. Ekaterinburg, Uralgeolkom, IGG UB RAS, 150-156. (In Russian)

16. Efimov A.A. (2010) Results of a 100-year study of the Platinum Belt of the Urals. litosfera, (5), 134-153. (In Russian)

17. Glikson A. (1980) Stratigraphy and evolution of primary and secondary greenstone complexes; data on the shields of the southern hemisphere. Rannyaya istoriya Zemli [Early history of the Earth]. Moscow, Mir Publ., 264-285. (In Russian)

18. Heuman L.M., LeCheminant A.N. (1993) Paragenesis and U-Pb systemstic of baddeleyite (ZrO 2 ). chem. Geol., 110, 95-126.

19. Hiroshi K., Kushiro I. (1993) Partial melting of dry peridotite at high pressure: Determination of composition of melts segregated from peridotite using aggregates of diamonds. Earth planet. sci. lett., 114, 477-489.

20. Ibragimova E.K., Rad’kov A.V., Molchanov A.V., Shatova N.V., Shatov V.V., Lepekhina E.N., Antonov A.V., Tolmacheva E.V., Solov’ev O.L., Terekhov A.V., Khorokhorina E.I. (2015) The results of U-Pb (SHRIMP II) dating of zircons from dunites of Inagli massif (Aldan Shield) and the problem of the genesis of concentrically zoned complexes. Regional. Geol. Metallogeny, (62), 64-78. (In Russian)

21. Ireland T.R., Williams I.S. (2003) Rev. Mineral. Geochim., 53, 215-241.

22. Ivanov O.K. (1997) Kontsentricheski-zonal’nye pirokse nitdunitovye massivy urala: mineralogiya, petrologiya, genesis [Concentrically zoned pyroxenite-dunite massifs of the Urals: mineralogy, petrology, genesis]. Ekaterinburg, URGU Publ., 488 p. (In Russian)

23. Kadik A.A., Stupakov E.P. (1970) Modeling of temperature fields near magmatic bodies with considerable radial extent. Geokhimiya, (1), 43-53. (In Russian)

24. Karetnikov A.S. (2006) Age and genesis of platinum mineralization of the Konder massif: paleomagnetic and radioisotope data. litosfera, (3), 96-107. (In Russian)

25. Knaupf O.V. (2009) U-PB age of zircons from duniteclinopyroxenite nuclei of Kytlymsky (Middle Urals) and Galmoenensky (South Koryakia) zonal massifs of the Ural type. Vestn. spbGu, (4), 64-71. (In Russian)

26. Krasnobaev A.A., Anikina E.V., Rusin A.I. (2011) Zirconology of dunite of the Nizhny Tagil massif (Middle Urals). Dokl. Earth sci., 436(2), 290-294.

27. Kulikova V.V., Bychkova Ya.V., Kulikov V.S. (2010) Baddeleyite is the main mineral for isotopic dating of mafic-ultramafic komatiite series of the southeastern Fenoscandian shield. “Sovremennaya mineralogiya: ot teorii k praktike”. Tezisy XI s”ezda Rossiiskogo mineralogicheskogo obshchestva [“modern mineralogy: from theory to practice”. Abstracts of the XI Congress of the Russian Mineralogical Society], 212-214. (In Russian)

28. Kuznetsov D.V., Mukatova A. (2013) The formation of baddeleyite during the disilication of zircon in the rodingitized highly granular granitites of the Mindyak massif in the Southern Urals. Ezhegodnik-2012. Tr. IGG UrO RAN [Yearbook-2012. Proc. IGG UB RAS], 160, 224-228. (In Russian)

29. Kuznetsov Yu.A. (1964) Glavnye tipy magmaticheskikh formatsii [The main types of magmatic formations]. Moscow, Nedra Publ., 387 p. (In Russian)

30. Lizuka T., Yamaguchi T., Hibiya Y., Amelin Y. (2015) Meteorite zircon constrains on the bulk Lu-Hf istope composition and early differentiation of the Earth. proc. Nat. acad. usa, 112(17), 5331-5336.

31. Lykov A.V. (1954) Yavleniya perenosa v kapillyarnoporistykh telakh [Transport phenomena in capillary-porous bodies]. Moscow, Gos. Izd. technical and theoretical literature Publ., 296 p. (In Russian)

32. Malitch K.N., Efimov A.A., Ronkin Yu.L. (2009) Archean U-Pb isotope age of zircon from dunite of the Nizhny Tagil massif (the Uralian Platinum belt). Dokl. Earth sci., 427(1), 851-855.

33. Malitch K.N., Efimov A.A., Badanina I.Yu. (2012) The age of Kondyor massif dunites (Aldan province, Russia): first U-Pb isotopic data. Dokl. Earth sci., 446(1), 1054-1058.

34. Mitsyuk S.S, Zinchuk N.N., Koptil’ V.N., Kutuzova E.Ya., Lashkevich I.V. (2005) New indicators of zircons of kimberlite origin. Geologiya almazov – nastoyashchee i budushchee [Geology of diamonds – present and future]. Voronezh, St.Univ. Publ., 674-720. (In Russian)

35. Moskaleva S.V. (1959) On the age and structure of the Kraka massifs in the Southern Urals. Dokl. Akad. Nauk SSSR, 127(1), 170-173. (In Russian)

36. Pinus G.V., Velinskii V.V., Lesnov F.P., Bannikov O.L., Agafonov L.V. (1973) Al’pinotipnye giperbazity Anadyro-Koryakskoi skladchatoi sistemy [Alpinotype hyperbasites of the Anadyr-Koryak fold system]. Novosibirsk, Nauka Publ., 320 p. (In Russian)

37. Pushkarev E.V., Fershtater G.B. (1995) Mineralogical and petrochemical discreteness of rocks and the problem of the origin of primary melts of dunite-clinopyroxenite-syenite-gabbro complexes. Aktual’nye problemy magmaticheskoi geologii, petrologii i rudoobrazovaniya [Actual problems of magmatic geology, petrology and ore formation]. Ekaterinburg, Uralgeolkom, IGG, UB RAS, 100-110. (In Russian)

38. Robie R.A., Hemingway B.S., Fisher J.R. (1978) Thermodynamic properities of minerals and related substances at 298.15K and 1 bar Pessure and at higher temperatures. Geol. surv. Bull., 1452, 456.

39. Ronkin Yu.L., Efimov A.A., Lepikhina G.A., Maslov A.V., Rodionov N.V. (2013) U-Pb dating of the baddeleyttezircon system from Рt-bearing dunite of the Konder massif, Aldan shield: new data. Dokl. Earth sci., 450(2), 607-612.

40. Ryzhkov V.M., Anfilogov V.N., Blinov I.A., Krasnobaev A.A., Valizer P.M. (2016) Phase equilibria in the mgO–SiO 2 –ZrO 2 system. Dokl. Earth sci., 469(2), 824-827.

41. Salop L.I. (1982) Geologicheskoe razvitie Zemli v dokembrii [Geological development of the Earth in the Precambrian]. Leningrad, Nedra Publ., 343 p. (In Russian)

42. Saltykov A.K., Nikitina L.P., Matukov D.I. (2008) U-Pb age of zircon from xenoliths of mantle peridotites in Cenozoic alkaline basalts of the Vitim plateau (Eastern Baikal region). Zapiski RMO, (3), 1-22. (In Russian)

43. Savel’ev D.E., Snachev V.I., Savel’eva E.N., Bazhin E.A. (2008) Geologiya, petrologiya i khromitonosnost’ gabbro-giperbasitovykh massivov Uzhnogo Urala [Geology, petrology and chromite content of gabbro-hyperbasite massifs in the Southern Urals]. Ufa, 319 p. (In Russian)

44. Savel’eva G.N., Batanova V.G., Berezhnaya N.A., Presnyakov S.L., Sobolev A.V., Skublov S.G., Belousov I.A. (2013) Polynchronous formation of mantle complexes of ophiolites (Polar Urals). Geotektonika, (3), 43-57. (In Russian)

45. Shulyatin O.G., Andreev S.I., Belyatskii B.V., Trukhalev A.I. (2012) Age and stage of formation of igneous rocks of the mid-Atlantic Ridge by geological and radiological data. Region. Geol. Metallogeny, 50, 28-36. (In Russian)

46. Simonov V.A., Kovyazin S.V., Prikhod’ko V.S. (2011) Gene sis of platiniferous massifs in the Southeastern Siberian platform. Petrology, 19(6), 549-567.

47. Simonov V.A., Puchkov V.N., Prikhod’ko V.S., Stupakov S.I., Kotlyarov A.V. (2013) Conditions of crystallization of dunites of the Nizhny Tagil platinum-bearing ultrabasic massif (the Urals). Dokl. akad. Nauk, 449(6), 692-695. (In Russian)

48. Skolotnev S.G., Ipat’eva I.S., Beltenev V.E., Lepekhina E.N. (2010) Younger and older zircons from rocks of the oceanic lithosphere in the central atlantic and their geotectonic implications. Geotectonics, 44(6), 462-492.

49. Takahashi E. (1986) Melting of dry peridotite KLB-1 up to 14 GPa: Implication on the origin of peridotitic upper mantle. J. Geophys. Res., 91, 9367-9382.

50. Toropov N.A., Barzakovski V.P., Lapin V.V., Kurzeva N.N. (1969) Diagrammy sostoyaniya silikatnykh system. Spravochnik. T. 1 [Diagrams of the state of silicate systems. Reference book. V. 1]. Leningrad, Nauka Publ., 822 p. (In Russian)

51. Velinskii V.V. (1979) Al’pinotipnye giperbasity perekhodnykh zon ocean–kontinent [Alpin-type hyperbasites of ocean–continent transition zones]. Novosibirsk, Nauka Publ., 264 p. (In Russian)


Рецензия

Для цитирования:


Anfilogov V.N., Krasnobaev A.A., Ryzhkov V.M. Ancient age of zircons and issues associated with the genesis of dunites from gabbro-ultrabasite complexes of orogenic areas and central-type platform massifs. Литосфера. 2018;18(5A):48-56.

For citation:


Anfilogov V.N., Krasnobaev A.A., Ryzhkov V.M. Ancient age of zircons and issues associated with the genesis of dunites from gabbro-ultrabasite complexes of orogenic areas and central-type platform massifs. LITHOSPHERE (Russia). 2018;18(5A):48-56.

Просмотров: 333


Creative Commons License
Контент доступен под лицензией Creative Commons Attribution 4.0 License.


ISSN 1681-9004 (Print)
ISSN 2500-302X (Online)