Alkaline rocks from Mariupol massif (SW Ukraine) part II

baner

September 2010 M.P.Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the National Academy of Science of Ukraine and the Mineralogical Society of Poland organized conference ALKALINE ROCKS: PETROLOGY, MINERALOGY, GEOCHEMISTRY Conference dedicated to the memory of J.A.Morozewicz.

Post-conference field trip took place in the Mariupol massif (Oktyabr’skii Massif), Azov Sea Region, Donetsk (Donets’k) Oblast’, SE Ukraine.

morozewicz_1The conference was dedicated to the memory of famous Polish geologist, petrographer, and mineralogist Joseph August Morozewicz (1865–1941), who made important contributions to the investigation of alkaline rocks. During the period 1898–1908, Morozewicz carried out investigations in the Azov region. He discovered and described (in papers in German, Polish, and Russian) the alkaline rocks of the Mariupol area, in particular mariupolites, albite–nepheline rocks. He found the new minerals taramite and beckelite (synonym of britholite-(Ce)) and determined a first composition for nepheline, known today as Morozewicz nepheline (Ne68Ks22Q10) [Elements, Vol.5 (6), 2009].

At 1929 Morozewicz published book Mariupolit i jego krewniaki = Mariupolite et ses parents (Mariupolite and its relatives in Polish and French). He described there rocks of the area: mariupolites, foyaites, syenites, pyroxenites, pegmatites and granites.

mariupolit-i-jego-krewniaki-1

On the map attached to the book, polish names are present. Mitrowka is called today Dmytriivka, Donske village is located between Sretenka and Apostołowka, near the big, blue spot of mariupolites, Lazarivka is located between Sretenka and Archangiełka, along the stream Lisica (mariupolites with magnetite) and river Wali-Tarama (taramitic foyaites), and Khlebodarivka quarry is located on the left edge of the map (marked with small triangle, left from Archangiełka village).

During the second day of two-day field trip there were another two stops (first day):

Dmitrievskii quarry is located in the vicinity of the Oktyabr’skii Massif and reveals alkaline apogranitic metasomatic rocks, albitites, albite-microcline rocks with considerable amount of aegerine, in some places with astrophylite and rich molibdenium mineralization. Rocks contain some zircon, britholite, bastnäsite, fluorite, pyrochlore.

dmytriivka
Dmitrievskii quarry, Oktyabr’skii Massif (Mariupol’skii), Azov Sea Region, Donetsk (Donets’k) Oblast’, Ukraine

Open pit in Donske village is located within the Oktyabr’skii Massif of alkaline rocks. Open pit exposes mariupolite, pegmatitic mariupolite with sodalite, nepheline syenite pegmatite, sodalite pegmatite. Mariupolite contains some britholite, pyrochlore and zircon.

donsky-kopia
Dumps around Donskoy quarry, Mazurovskoe Zr deposit, Oktyabr’skii Massif (Mariupol’skii), Azov Sea Region, Donetsk (Donets’k) Oblast’, Ukraine
References:
Morozewicz J.A. (1929): Mariupolit i jego krewniaki = Mariupolite et ses parents. – Prace Pol. Inst. Geol.: 151 pp.
Kryvdik S.G. (2002): Metallogeny of Alkaline Complexes of the Ukrainian Shield. Mineral. Journ. (Ukraine): 24(2/3): 58-64.
Krivdik S.G., Nivin V.A., Kul’chitskaya A.A., Voznak D.K., Kalinichenko A.M., Zagnitko V.N., Dubyna A.V. (2007): Hydrocarbons and other volatile components in alkaline rocks from the Ukrainian Shield and Kola Penisula. Geochemistry International: 45 (3): 270–294.
Dumańska-Słowik M., Sikorska M., Heflik W. (2011): Dissolved-recrystallized zircon from mariupolite in the Mariupol Massif, Priazovje (SE Ukraine). Acta Geologica Polonica: 61 (3): 277–288.
Dumańska-Słowik, M., Budzyń, B., Heflik, W., Sikorska, M. (2012): Stability relationships of REE-bearing phosphates in an alkali-rich system (nepheline syenite from the Mariupol Massif, SE Ukraine). Acta Geologica Polonica: 62: 247–265.
Ponomarenko A.N, Kryvdik S.G., Grinchenko A.V. (2013): Alkaline rocks of the Ukrainian Shield: Some mineralogical, petrological and geochemical features. Mineralogia: 44 (3-4): 115-124.
Voznyak D.K., Chernysh D.S., Melnikov V.S., Ostapenko S.S. (2013): Baddeleyite segregations in zircon of the Azov zirconium-rare-earth deposit (Ukrainian Shield). Mineralogia: 44 (3-4): 125-131.
Dumańska-Słowik M., Heflik W., Kromska A., Sikorska M. (2015): Sodic fenites of the Oktiabrski Complex exposed in the Khlibodarivka quarry (East Azov, SE Ukraine): reconstruction of their growth history. N. Jb. Geol. Paläont. Abh.:275/3: 269–283.
Sharygin, V.V. (2015): Zincian micas from peralkaline phonolites of the Oktyabrsky massif, Azov Sea region, Ukrainian Shield. European Journal of Mineralogy: 27(4): 521-533
Dumańska-Słowik M., Heflik W. (2016): Skały ultrazasadowe i zasadowe z otoczenia mariupolitów występujących w alkalicznym Masywie Oktiabrskim (SE Ukraina) – badania wstępne. Gospodarka surowcami mineralnymi – Mineral resources management: 32 (2), 63–78.
Dumańska-Słowik, M., Pieczka, A., Heflik, W., Sikorska, M. (2016): Cancrinite from nepheline syenite (mariupolite) of the Oktiabrski massif, SE Ukraine, and its growth history. Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy: 157: 211-219.

Zr-bearing minerals

Zirconium is a chemical element with symbol Zr and atomic number 40. The name of zirconium is taken from the name of the mineral zircon, the most important source of zirconium. The word zircon comes from the Persian word zargun زرگون, meaning “gold-colored”. Zirconium is a lustrous, grey-white, strong transition metal that resembles hafnium and, to a lesser extent, titanium.

The principal commercial source of zirconium is zircon [ZrSiO4]. As of 2013, two-thirds of zircon mining occurs in Australia and South Africa. Zircon resources exceed 60 million tonnes worldwide and annual worldwide zirconium production is approximately 900,000 tonnes. Zirconium also occurs in more than 140 other minerals, including the commercially useful ores baddeleyite [ZrO2] and kosnarite [KZr2(PO4)3].