Journals / Maden Tetkik ve Arama Dergisi / 1991 / Cilt: 113 - Sayı: 113

GEOLOGICAL SETTING, DISTRIBUTION AND FORMATION OF KIRKA (SEYİTGAZİ-ESKİŞEHİR) BORATE DEPOSITS

Pages
63–64
Publication Date
1991-06-01
DOI
—
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AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

Borate minerals were formed by different processes such as synsedimentary, authigenesis and diagenetic transformation, according to their shapes/forms and kinds.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:Middle-Upper Miocene aged borate deposits in the Kırka basin having volcano sedimentary lacustrine rocks are found within the dolomitic claystone/marls as lense shaped.
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Key Findings & Data:Borate deposits situated in the two parts of the region were separated by paleotopographic threshold consisting of basement rocks and/or vertical blocking movements.
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Conclusion & Impact:Borate minerals were formed by different processes such as synsedimentary, authigenesis and diagenetic transformation, according to their shapes/forms and kinds.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters

Abstract

Middle-Upper Miocene aged borate deposits in the Kırka basin having volcano sedimentary lacustrine rocks are found within the dolomitic claystone/marls as lense shaped. The most lower and upper parts of the deposit are surrounded by carbonaceous rocks. Borate deposits situated in the two parts of the region were separated by paleotopographic threshold consisting of basement rocks and/or vertical blocking movements. Borate minerals show vertical and lateral mineralogical zonation such as Na, NaCa and Ca-borate in the southeastern area of the basin (Sarıkaya), whereas Ca-borate is represented only in the northwestern area (Göcenoluk). Borate minerals were formed by different processes such as synsedimentary, authigenesis and diagenetic transformation, according to their shapes/forms and kinds.

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Cite This Article

YALÇIN, H., BAYSAL, O. (1991). GEOLOGICAL SETTING, DISTRIBUTION AND FORMATION OF KIRKA (SEYİTGAZİ-ESKİŞEHİR) BORATE DEPOSITS. Maden Tetkik ve Arama Dergisi, Cilt: 113 - Sayı: 113, 63–64. https://ajindex.com/articles/54313

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References (6)

  1. Arda, T., 1969. Kırka-Sarıkaya boraks yatağının jeolojik etüdü: MTA Rap., 4158 (yayımlanmamış), Ankara.
  2. Aristarian, LF. ve Hurlbut, Jr. C.S., 1972, Boron minerals and deposits. Part I Lses. Distribution and economic minerals of boron: Min. Record. 3. 165-172.
  3. Ataman, G., 1966, Geochimie des mıneraux argıleux dans les bassins sedimentaires marins. Etudes sur lc bassın Triassiquc du Jura: Mem. Serv. Carte Geol. Als. Lorr, 25. 237s., 1967, La geochimie du bore et du gallium dans les mıncraux argıllcux: Chem. Geol., 2, 297-307. ve Baysal, O., 1973, Bazı bor minerallerinin termik reaksiyonları ve bunların atom yapısına etkisi: Cumhuriyetin 5ü. Yıl ı Yerbilimleri Kong. Bült. MTA Yayl., 537-565. ve, 1978, Clay mineralogy of Turkish borate deposits: Chem Geol., 22, 233-247
  4. Baysal, O., 1972a. Sankaya (Kırka) borat yataklarının mineralojik ve jenetik incelenmesi: Doçentlik tezi, H.Ü Müh Fak, 157s. (yayımlanmamış), Beytepe, Ankara., 19726, Sankaya (Kırka) boratlarında yeni bir stronsiyum borat minerali: Tunelit: M'I'A Derg. 79, 22-30., 1973a. Sankaya (Kırka) borat yataklarının oluşumu: Türkiye Mad Bil. Tek III. Kong. 255 277., 19736, Türkiye'deki yeni bulunan sulu magnezyum-borat mineralleri: Kumakova, inderit, inderborit: MTA Derg., 80, 89-99., 1974, Kırka borat yataklarındaki kil mineralleri üzerine ön çalışma: Türkiye Jeol. Kur. Bull, 17. 17-30. ve Ataman, G., 1975, Türkiye'de yem bir bor minerali: Kemit ve oluşumunun tartışması: Türkiye Jeol. Kur. Bült., 18, 3-10.
  5. Bowser, C.J., 1964, Geochemistry and petrology of the sodium borates ın the non-marinc evaporite envıronment: Ph. D. Dissertation, University of Califomia, Los Angeles, l10s Christ, C.L., 1960, Crystal chemistry and Systematic dassification of hydrate borate minerals: Amer. Min., 45. 334-340.;
  6. Clark, J.R. ve Evans, H.T.Jr., 1958, Studies of borates minerals (III): The crystal structure of Colemanite, CaB3O4 (OH) 3H2O: Acta. Cryst., 11.761-770. ve Garrels, R.M., 1959, Relations among sodium borate hydrates at Kramer deposits, Boron, Califomia: Amer. J. Sci., 257, 516-528. ve Clark, J.R., 1960. Studies of borate minerals (IX): The crystal structure of meycrhofferite, CaB3O3 (OH)5.H2O: Z. Krist., 114, 321 - 342.; Truesdell, A.H ve Erd, R.C., 1967, Borate mineral assemblages ın the system Na2O-CaO-MgO-B2O3 -H2O: Geochim. Cosmochim Acta, 31, 313-337. ve Hostetler, P.B., 1970, Studies in the system MgO-SiO--CO2 -H2O (II): The aclivity-product constant of magnesite: Amer. J. Sci., 268.439-453. Cla