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Manisa-Gördes rutil yataklarının oluşumu ve jeolojisi

Başlık çevirisi mevcut değil.

  1. Tez No: 29746
  2. Yazar: NURDAN YAĞCI
  3. Danışmanlar: PROF. DR. ERDİNÇ KİPMAN
  4. Tez Türü: Yüksek Lisans
  5. Konular: Jeoloji Mühendisliği, Geological Engineering
  6. Anahtar Kelimeler: Belirtilmemiş.
  7. Yıl: 1993
  8. Dil: Türkçe
  9. Üniversite: İstanbul Üniversitesi
  10. Enstitü: Fen Bilimleri Enstitüsü
  11. Ana Bilim Dalı: Jeoloji Mühendisliği Ana Bilim Dalı
  12. Bilim Dalı: Belirtilmemiş.
  13. Sayfa Sayısı: 98

Özet

ÖZET Manisa iline baql ı Gördes - Demirci ilçeleri arasında yer alan çalışma alanı, Türkmen Dağının kuzeyinde Bardakçı köyünden başlar, güneyde Kahve Mahallesi 'ne kadar devam eder. Batıda Kulalar Bağcılar Köyü. doğuda da Uiacık Rahmanlar Köyü sınır teski 1 eder. Menderes Masifi 'nin Gördes Asmasifi uetaıorf itleri sahanın temelini oluşturur. Metaraorf it birimleri pegmatoid ve kuvars damarları keser. Tüm birimleri Neoien yaşlı sedimentler uyumsuz olarak örter. Metamorfik topluluğun büyük kesimi mi qmatiklesmi ş az bir kısmı ise kendini korumuştur. Gördes Asmasifinde çalışan dıger araştırmacıların

Özet (Çeviri)

SUMMARY This research covers the area between Gördes and Eiemirci provinees in the Manisa muni ci pol i ty The above mentioned area strats from Bardakci Village which is north to Turkmen Peak and continues to Kahve district. The western boudary of the area starts from Kulalar. Begenler Village and continues to the Ulacik, Rahmanlar village in the east. Sordes Asmasive of Menderes Massive is the foundatior of metamorphite area. Metamorphic units are cut by pegmatoid and quartz veins. While units are covered by Neocene aged sedyments in an irregular manner. A great portion of meta- morfic is mi groat i t i zed and a small portion was preserved other researchers who studied Gördes Asmasiwe (Dag 1988) have determined that metamorphic rock of this area are sedi- mantary origin. This has been determined by width length measure merits. Pepmatiid veins lie in NE-SW and E-W direct ions. The width is ot these veins are 25 - 30 ms.And their leng ths are measured in kilometers their composition is Na- teldspath + guortz + muskoxite + biotit + turmalin and granat in E-W direction veins there is Be. In both directions there is no zoning both they are composed at simple pegmatoi ds. NE- SW direction pegmatoid veins (plaj) is aboundent and its com position is albite olipoctass. In E-W direction pegmatoids K-feldispath unite composition ortokles is abundent NE-SW and E-W pegmatoid veins which are crops of the same granitic mog- ra are formed under high hydrother mal -pegmati t i c conditions. In the classification at the massive dene by taking the temperature as criterium. metamarphism starting garnet-musko xite-guartz schist with low temperature continues in low parts with the appereance of sliraarite and distehen in sillimanite -garnet- disthen schist and reaches the high temperature zone of the avarage degree. When we come to the layered gnays at the lowest level we reach high degree metamor phism. Granitic material has approached metamorphic series as rock veins at various levels pegmatoids rich in muskoxite and -v-feldispath has been farmed as the last creg of granitic mete- rial. There are plastic deformations in the zone together with metamor phes i s and there are horizontal and izolinal folds. In depression areas which are formed by extension. As the temperatuve increases further. Because at the anatecsis and miqinatization starting with the further increasing of temperature verywide and granitic material accumulates at the bottom and a big part of sillimant garart and some part of gnays turns to migmatide. Technics neogen aged sediments have settled. In the investigation area there are guartz veins apart from feldispat rich pegmatoids. In these veins there are mus- coit. turmoline, rutile minerals. Besides it was determined that heavy minerals in detritic sediments of fluyatif origin which were feeded with the decoiftposi t i on an transportation of metamorfik units and magma- tic rocks, show a change as a function of density difference. Petrografic investigations has demonstrated the presence of mi nerals like granat, rutile, magnetit, ilmetit. turmolin. dişten zircon, hematite. Rutil has taken its place in fine dimensioned sediments as a result of decomposition and carrying at metamorfic units. Rutil whichis of gravel and big.gravel dimension is in guartz veins in approaching higher layers and reaching until meta- morphic rocks have resulted in rutil rich in Ti. In sillimat garar t-di sten schist there are bigger rutil minerals. With the decomposition of these rocks they have been added to river pi aser s. The distance of the particles with sharp edges to guartz veins are lesser. The particules carried furthe are more rounded and smaller shape. In general since rutil is of form of chanel fill it forms zones parallel to channel. -VI-

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