MINERALOGY OF THE MADENBELENITEPE (SOĞUKPINAR-BURSA) TIN MINERALIZATION

Yıl 1979, Cilt: 92 Sayı: 92 , 25 - 35 , 01.09.1979

Ahmet Çağatay Yılmaz Altun Bülent Arman

https://izlik.org/JA73ZK24TH

Öz

Tin mineralization occurs in the greisenized granite porphyry in Madenbelenitepe area. Stannite
is the major tin mineral. Cassiterite is found in trace amounts. Associated minerals are arsenopyrite, pyrite, sphalarite,
fahlerz (tennantite-tetrahedrite), galena, chalcopyrite, bournonite, boulangerite, rutile and pyrrhotite. Gangue minerals
are represented by quartz, muscovite, sericite and minor amounts of apatite.
To the East of Madenbelenitepe mineralization, scheelite, wolframite and molibdenite occurs in granite, greisenized
granite and granite porphyry. Pyrite, arsenopyrite, cosalite, scheelite, wolframite (partly altered to scheelite), molibdenite,
specularite, sphalarite, tennantite, chalcopyrite and tourmaline occurs in hydrothermal quartz veins intersecting
granites and metamorphic schists.
Madenbelenitepe tin mineralization shows many features similar to those observed in the upper zones of other
tin mineralizations found throughout the world, and the mineralization described here, is seemingly a «hydrothermal
quartz greissem type formed at high temperatures.

Anahtar Kelimeler

MINERALOGY , MADENBELENITEPE , SOĞUKPINAR-BURSA

MADENBELENİTEPE (SOĞUKPINAR-BURSA) KALAY CEVHERLEŞMESİNİN MİNERALOJİSİ

https://izlik.org/JA73ZK24TH

Öz

Madenbetenitepe kalay cevherleşmesi grayzenleşmiş granitporfir içinde bulunmaktadır. Kalay mineralleri olarak fazla stannit, yanında eser miktarda kassiterit izlenmiştir. Diğer maden mineralleri olarak arsenepirit, pirit, sfalerit, fahlerz (tennantit-tetraedrit), gelenit, kalkopirit, bournonit, bulanjerit, rutil ve pirotin bulunmaktadır. Kuvars, muskovit, serisit ve tali mineral olarak apatit gözlenen başlıca gang mineralleridir. Madenbelenitepe cevherleşmesinin doğu kesiminde granit, grayzenleşen granit ve granitporfir içinde şelit, volframit, molibdenit ile bu kayaç ve metamorfik şistleri kesen hidrotermal kuvars damarlarında pirit, arsenopirit, kosalit, şelit, volframit (kısmen şelite dönüşmüş), molibdenit, spekülarit, sfalerit, tennantit, kalkopirit ve turmalin izlenmektedir. Madenbelenitepe kalay cevherleşmesi, içinde bulunduğu ortam yönünden yerkürede bilinen kalay yataklarının üst zonlarına benzerlik göstermekte ve yüksek ısılarda oluşmuş «hidrotermal kuvars grayzen» tipinde bir yatak görünümü vermektedir. 

Anahtar Kelimeler

MADENBELENİTEPE , SOĞUKPINAR-BURSA , CEVHERLEŞMESİNİN MİNERALOJİSİ

Kaynakça

• Aubert, G., 1969, Les coupoles granitiques de Montebras et Echassieres (Massif Central, Français) et la genese de leurs mineralisations en etain, lithium, tungstene et beryllium: Memoires du B.R.G.M (Bureau de Recherches Geologigues et Minieres), 46 (2 cilt), Paris.
• Baumann, L; Stemprok, M.; Tischendorf, G. ve Zoubek, V., 1974, Metallogeny of tin and tungsten in the Krusne Hory-Erzgebirge: internal. Geological Correlation Programme, Excursion Guide, Prag.
• Bromley, A.V., 1975, Tin mineralization of Western Europe: is it related to crustal subduction ? Institution of Mining and Metallurgy, Transactions/ Section B (Applied earth Science), London, B 28 - B 30.
• Burnol, L., 1974, Acid granites and associated metallization in the North-Western part of the French Central Masse: International Geological Correlation Programme, Metallization associated with acid magmatism, Symposium Karlovy Vary, 59.76.
• Deer, W.A.; Howie, R.A: ve Zussman, J., 1962, Rock-ferming minerals: 3, Longman, London, 90.
• Fox, D.J., 1969, Tin mining iri Spain and Portugal.-a paper of informatioh.- Fox, W. editör, A Second technical conference on tin, Volume one, Bangkok, 223-265.
• Hasking, K.F.G., .1970, The nature of the primary tin orts of the southw!est of England: Fox, W editör, A second technical conferencç on tin. Volume three, International tin Council, London, 1157-1244.
• Levy, CL., ,1956, La stannite jaune du gisement de Vaulry, Haute Vieane: Bull. Soc. franc. Min. 79, Paris, 383-391.
• ——1966, Contribution â la mineralogie des sulfures de cuivre du type Cuax S4: Mem. Bur. Rech. Geol. et Minieres. Der A 4652, 5499, 158.
• —-—- ve Prouvost, J., 1957, Rapport entre la chalcopyrite, la stannite et la renierite: Bull. Soc. fr. Mineral. 8,59-66.
• Mitchel, A.H.G., 1974, Southwest England granites: magmatism and tin mineralization in a post collision tectonic ,sating: Instition of .Mining and Metallurgy, Transactions / Section B (Applied earth Science) London, August, B95 - B97.
• Moh, G.H., 1960, Experinıentelle .Untersuchungen an Zinnkieşen und analogen Germanium verbindungen: N. Jahrb. Min. Abh., 94, Festband Ramdohr, 1125-1146.
• ,1961, Neue Untersuchungen der Mineralgruppen Zinnkies-Fahlerz: Fortsch, d. Mineralogie, 39,352.
• ,1969, The tin-sulfur system and related minerals: N. Jahrb. Miner., 111, 227-263.
• ve Ottemann, J., 1962, Neue Untersuchungen an Zinnkiesen und Zinnkiesverwandten: N. Jahrb. 99, 1-28.
• MulUgan, R., 1975, Geology of Cannadian tin Occurrences: Geological survey of Canada. Economic geology report, 2S,Ottawa, 1-129.
• Ramdohr, P., 1975, Die Erzmineralien und ihre Verwachsungen: 4., bearbeitete und erweiterde Auflage: Akademie Verlag Beklin, 587^603.
• Sçhröcke, H., 1968, Zur Bildung von Zinn-Wolfram-Lagerstatten. Eine Bemerkung: Mineralium Deposita, 3, Ber- .lin-Heidelberg, New York, 182-l84.
• Shcherba, G.N., 1970, Greisens (Part 1,2): internal: Geology Review, Washington, D.C. 114-150 >vc 239-255.
• Smirnov, V.I., 1976, Geology of mineral deposits: Mir Publishers, Moscow, 205-210.
• Stemprok, M., 1965, On the relation of tin-tungsten-molybdenum ore deposition to granites: Krystalinikum 3> Prag, 163-181.
• ,1971, Intra-Mineralization granitic dykes in the Krusne Hery metallogenic province: Krystalinikum,8, Prag, 141-148.
• Tischendorf, G., 1969, Über die kausalen Beziehungen zwischen Granitoiden und endogenen Zinnlagerstâtten: Zeitschrift f. angewandte Geologie, 15, Berlin 1969, 333-342.
• — , 1970, Zur .geochemischen Spezialisierung.der Granite des westerzgebirgischen Teilplutons: Geologie, 19, Berlin 1970, 25-40.
• — , 19J3, The .metaltogenic basis of tin exploration in the Erzgebirge: Transactions, Institution of Mining and Metallurgy, 82, B 9-B 24.
• Yajima, J. ve Ohta. E., 1979, Two-stage mineralization and formation process of the Toyoha Deposits, Hokkaido: Japan,,Mining Geology, 29 (5)., 291-306.