Osku County, East Azerbaijan Province, Irani
| Regional Level Types | |
|---|---|
| Osku County | County |
| East Azerbaijan Province | Province |
| Iran | Country |
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Neighbouring regions:
Locality type:
Other/historical names associated with this locality:
ShahrestÄn-e OskĆ«
Other Languages:
French:
préfecture d'Osku, Azerbaïdjan oriental, Iran
Italian:
shahrestÄn di Osku, Azerbaigian Orientale, Iran
Arabic:
Ù
Ùۧ۷ŰčŰ© ŰŁŰłÙÙ, ۣ۰۱ۚÙŰŹŰ§Ù Ű§Ùێ۱ÙÙŰ©, Ű„Ù۱ۧÙ
Azeri:
ĂskĂŒ ĆÉhristanı, ĆÉrqi AzÉrbaycan ostanı, Ä°ran
Dutch:
Osku County, Oost-Azerbeidzjan, Iran
Farsi/Persian:
ŰŽÙ۱۳ŰȘŰ§Ù Ű§ŰłÚ©Ù, ۧ۳ŰȘŰ§Ù ŰąŰ°Ű±ŰšŰ§ÛŰŹŰ§Ù ŰŽŰ±ÙÛ, ۧÛ۱ۧÙ
Finnish:
Osku, ÄzÄrbÄyjÄn-e SharqÄ«, Iran
Gilaki:
ŰŽÙ۱۳ŰȘŰ§Ù Ű§ŰłÚ©Ù, ۧÙ۱ۧÙ
Irish Gaelic:
Contae Osku, An IarĂĄin
Japanese:
ăȘăčăŻăŒéĄ, æ±ăąăŒă¶ă«ăăŒă€ăžăŁăŒăłć·, ă€ă©ăł
Pashto:
Ű§ŰłÚ©Ù ÙÙŰłÙۧÙÙ, ŰŻ Ù
ێ۱ÙÙ ŰąŰČ۱ۚۧÙŰŹŰ§Ù ÙÙۧÛŰȘ, ۧÙ۱ۧÙ
Serbo-Croatian:
Okrug Usku, IstoÄni AzarbajdĆŸan, Iran
South Azerbaijani:
ۧÙŰłÚ©Ù ŰšŰ€ÙÚŻÙâŰłÛ, ێ۱ÙÛ ŰąŰ°Ű±ŰšŰ§ÛŰŹŰ§Ù Ű§ÙŰłŰȘۧÙÛ, ۧÛ۱ۧÙ
Tajik (Cyrillic Script):
ĐšĐ°ÒłŃĐžŃŃĐŸĐœĐž ĐŁŃĐșÓŻ, ĐŁŃŃĐŸĐœĐž ĐĐ·Đ°ŃĐ±ĐŸĐčÒ·ĐŸĐœĐž ŃĐ°ŃÒÓŁ, ĐŃĐŸĐœ
Turkish:
Osku Ćehristanı, DoÄu Azerbaycan Eyaleti, Ä°ran
Urdu:
ŰŽÛ۱۳ŰȘŰ§Ù Ű§ŰłÚ©Ù, Ű”ÙŰšÛ ŰąŰ°Ű±ŰšŰ§ŰŠÛŰŹŰ§Ù ŰŽŰ±ÙÛ, ۧÛ۱ۧÙ
Welsh:
Sir Osku, Iran
Western Punjabi:
ŰŽÛ۱۳ŰȘŰ§Ù Ű§ÙŰłÚ©Ù, Ű”ÙŰšÛ ÚÚۯۧ ŰąŰČ۱ۚۧۊ ۏۧÙ, ۧÛ۱ۧÙ
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Rock Types Recorded
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| â 'Alkali Feldspar' Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â Analcime Formula: Na(AlSi2O6) · H2O Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â 'Biotite' Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â Diopside Formula: CaMgSi2O6 Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413.; Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â Diopside var. Salite Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413.; Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â 'Fayalite-Forsterite Series' Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â 'Glass' Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â 'K Feldspar' Formula: KAlSi3O8 Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â Leucite Formula: K(AlSi2O6) Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â 'Leucite phonolite' Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â Magnetite Formula: Fe2+Fe3+2O4 Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â Magnetite var. Titanium-bearing Magnetite Formula: Fe2+(Fe3+,Ti)2O4 Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â Nepheline Formula: Na3K(Al4Si4O16) Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â Phlogopite Formula: KMg3(AlSi3O10)(OH)2 Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
| â Sanidine Formula: K(AlSi3O8) Reference: Moine-Vaziri, H., Khalili-Marandi, S., & Brousse, R. (1991). Importance d'un volcanisme potassique, au MiocĂšne supĂ©rieur, en Azerbaidjan (Iran). Comptes rendus de l'AcadĂ©mie des sciences. SĂ©rie 2, MĂ©canique, Physique, Chimie, Sciences de l'univers, Sciences de la Terre, 313(13), 1603-1610.
Le Maitre, R. W., Streckeisen, A., Zanettin, B., LeBase, M. J., Bonin, B., Batemen, P., ... & Lameyre, J. 2002, Igneous rocks: A classification and glossary of Terms.
Moayyed, M., Moazzen, M., Calagari, A. A., Jahangiri, A., & Modjarrad, M. (2008). Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslamy peninsula, NW Iran: Implications for deep-mantle metasomatism. Chemie der Erde-Geochemistry, 68(2), 141-154.
Stocklin, J., & Nabavi, M. H. (1973). Tectonic map of Iran. Geological Survey of Iran, Tehran.
Pang, K. N., Chung, S. L., Zarrinkoub, M. H., Lin, Y. C., Lee, H. Y., Lo, C. H., & Khatib, M. M. (2013). Iranian ultrapotassic volcanism at~ 11 Ma signifies the initiation of postâcollisional magmatism in the A rabiaâE urasia collision zone. Terra Nova, 25(5), 405-413. |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 4 - Oxides and Hydroxides | |||
|---|---|---|---|
| â | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| â | var. Titanium-bearing Magnetite | 4.BB.05 | Fe2+(Fe3+,Ti)2O4 |
| Group 9 - Silicates | |||
| â | Analcime | 9.GB.05 | Na(AlSi2O6) · H2O |
| â | Diopside | 9.DA.15 | CaMgSi2O6 |
| â | var. Salite | 9.DA.15 | CaMgSi2O6 |
| â | Leucite | 9.GB.05 | K(AlSi2O6) |
| â | Nepheline | 9.FA.05 | Na3K(Al4Si4O16) |
| â | Phlogopite | 9.EC.20 | KMg3(AlSi3O10)(OH)2 |
| â | Sanidine | 9.FA.30 | K(AlSi3O8) |
| Unclassified Minerals, Rocks, etc. | |||
| â | 'Alkali Feldspar' | - | |
| â | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| â | 'Fayalite-Forsterite Series' | - | |
| â | 'Glass' | - | |
| â | 'K Feldspar' | - | KAlSi3O8 |
| â | 'Leucite phonolite' | - | |
| â | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | â Phlogopite | KMg3(AlSi3O10)(OH)2 |
| H | â Analcime | Na(AlSi2O6) · H2O |
| H | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| O | Oxygen | |
| O | â Leucite | K(AlSi2O6) |
| O | â Phlogopite | KMg3(AlSi3O10)(OH)2 |
| O | â Nepheline | Na3K(Al4Si4O16) |
| O | â K Feldspar | KAlSi3O8 |
| O | â Analcime | Na(AlSi2O6) · H2O |
| O | â Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| O | â Sanidine | K(AlSi3O8) |
| O | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| O | â Magnetite var. Titanium-bearing Magnetite | Fe2+(Fe3+,Ti)2O4 |
| O | â Diopside | CaMgSi2O6 |
| O | â Magnetite | Fe2+Fe23+O4 |
| F | Fluorine | |
| F | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Na | Sodium | |
| Na | â Nepheline | Na3K(Al4Si4O16) |
| Na | â Analcime | Na(AlSi2O6) · H2O |
| Na | â Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mg | Magnesium | |
| Mg | â Phlogopite | KMg3(AlSi3O10)(OH)2 |
| Mg | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Mg | â Diopside | CaMgSi2O6 |
| Al | Aluminium | |
| Al | â Leucite | K(AlSi2O6) |
| Al | â Phlogopite | KMg3(AlSi3O10)(OH)2 |
| Al | â Nepheline | Na3K(Al4Si4O16) |
| Al | â K Feldspar | KAlSi3O8 |
| Al | â Analcime | Na(AlSi2O6) · H2O |
| Al | â Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Al | â Sanidine | K(AlSi3O8) |
| Al | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Si | Silicon | |
| Si | â Leucite | K(AlSi2O6) |
| Si | â Phlogopite | KMg3(AlSi3O10)(OH)2 |
| Si | â Nepheline | Na3K(Al4Si4O16) |
| Si | â K Feldspar | KAlSi3O8 |
| Si | â Analcime | Na(AlSi2O6) · H2O |
| Si | â Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | â Sanidine | K(AlSi3O8) |
| Si | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Si | â Diopside | CaMgSi2O6 |
| K | Potassium | |
| K | â Leucite | K(AlSi2O6) |
| K | â Phlogopite | KMg3(AlSi3O10)(OH)2 |
| K | â Nepheline | Na3K(Al4Si4O16) |
| K | â K Feldspar | KAlSi3O8 |
| K | â Sanidine | K(AlSi3O8) |
| K | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Ca | Calcium | |
| Ca | â Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Ca | â Diopside | CaMgSi2O6 |
| Ti | Titanium | |
| Ti | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Ti | â Magnetite var. Titanium-bearing Magnetite | Fe2+(Fe3+,Ti)2O4 |
| Fe | Iron | |
| Fe | â Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Fe | â Magnetite var. Titanium-bearing Magnetite | Fe2+(Fe3+,Ti)2O4 |
| Fe | â Magnetite | Fe2+Fe23+O4 |
Geochronology
Mineralization age: Miocene : 11.0 ± 0.1 Ma to 10.7 ± 0.2 MaImportant note: This table is based only on rock and mineral ages recorded on mindat.org for this locality and is not necessarily a complete representation of the geochronology, but does give an indication of possible mineralization events relevant to this locality. As more age information is added this table may expand in the future. A break in the table simply indicates a lack of data entered here, not necessarily a break in the geologic sequence. Grey background entries are from different, related, localities.
| Geologic Time | Rocks, Minerals and Events | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| Phanerozoic | ||||||||||
| Cenozoic | ||||||||||
| Neogene | ||||||||||
| Miocene |
| |||||||||
Fossils
This region is too big to display the fossil list, try looking at smaller subregions.Other Databases
| Wikipedia: | https://en.wikipedia.org/wiki/Osku_County |
|---|---|
| Wikidata ID: | Q1291748 |
| GeoNames ID: | 449426 |
Localities in this Region
- East Azerbaijan Province
- Osku County
Other Regions, Features and Areas that Intersect
Eurasian PlateTectonic Plate
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