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Kil Minerallerinin Diyajenetik ve Ortamsal Nitelikleri

Diagenetic and environmental properties of the clay minerals

Journal Name:

  • Jeoloji Mühendisliği Dergisi

Publication Year:

  • 1984
Author NameUniversity of AuthorFaculty of Author
Abstract (2. Language): 
Magnetic a»d environ-mental properties of the day mineral» ape vartaMe, The major diage nette phase diagrams of the argillaceous sediments and sedimentary rock faciles ûave been established by thi chemical dates of the natural phylloâlHcates, The presence erf glauciOTiite is a usefiil criteria for the mariai and shalow imarine sedîm^ts and is not affected much fey the burial diiagenesas. Chlorite» are f&mmû b} weathering of the primary micas .They replaces ilites and otheiF <Oay minerals at the advanced stages o ûlagenesis, speeîfloaliy at the beglimlnf of metamorphtem, Smectttes are exposed to Important mtaeralogica thages which extend from the beginning of sedimentation to late stage of diagenesis. The iDceurenoe of chio rites In the sedimentary rocks M controlled by the other phases rather than their thermal stabMJty; the: Câisappêar at toe late stage of metamorph&m. lllltes form through a series of chemical reactions unde different P « T conditions.
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Abstract (Original Language): 
Kil minerallerinin diyajenetik ve ortamsal nitelikleri değişkendir. Killi çökeller ile çökel kaya fasiyeslerinm ana diyajenetik faz diyagramları, tabii filloslikatların kimyasal verilerine dayanılarak kurulmak, tadır, Glokonit denizel ve daha çok sıf denizel kökenli gökeîier îgin yararlı bir ayırag olup gömülme diyajene^ zinden fazlaca etkilenmez, Klorit birincil mikaların ayrışma ürünü olarak gelişir, Diyajenezin ileri safhalarmda özellikle metamorfizmaya eri§tifi durumlarda illit .ye elif er kil minerallerini ornatır, Sîmektitler ise sedimantasyondan ileri diyajenez evresine kadar önemli mineralojik defişimlere uğrarlar, Klorİtin sedimanter kayalar içerisinde bulunuşu, bunun termal duraylılığından gok diğer fazların etkisinde olup ileri metamorfizma evresinde tümüyle yok olur. îllit degigik P=T şartları altında bir seri kimyasal reaksiyonlar ile oluşur.
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39-44
  • Turkish

REFERENCES

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