SEDIMENTARY CHARACTERISTICS OF THE DIKMENDEDE FORMATION (ANKARA, TURKEY)
Küçük Resim Yok
Tarih
2011
Yazarlar
Dergi Başlığı
Dergi ISSN
Cilt Başlığı
Yayıncı
INT SCIENTIFIC CONFERENCE SGEM
Erişim Hakkı
info:eu-repo/semantics/closedAccess
Özet
The Maastrichtian aged Dikmendede Formation in the Orhaniye (Kazan-Ankara) area formed in a deep-marine environment. The formation consists of alternating green, grey-coloured turbiditic conglomerate, sandstone, shale, claystone and marl. The unit has typical flysch features and has sedimentary structures such as thin/thick bedding, normal graded bedding, erosional surfaces, flute casts, load structures, ball-and-pillow structures, bounce marks, slump structures and numerous biogenic traces. The conglomerates of turbiditic channel fills display clast imbrication and graded bedding. The sandstones of the Dikmendede Formation are mainly made of quartz, plagioclase, alkali feldspar (orthoclase, microcline, sanidine), sedimentary (carbonate, chert, sandstone, shale), metamorphic (micaschist, quartzschist, calcschist, phyllite, gneiss), volcanic rock clasts, mica (muscovite, biotite), heavy minerals (epidote, opaque minerals, glaucophane, piroksen, rutile, turmaline). The sandstones, texturally and mineralogically immature, are cemented by calcite and iron-oxides, in addition to clayey (illite, smectite, chlorite) and in a lesser amount micritic matrix.
Açıklama
11th International Multidisciplinary Scientific GeoConference -- JUN 20-25, 2011 -- Albena, BULGARIA
Anahtar Kelimeler
Orhaniye, Dikmendede, sandstone, flysch, flute cast
Kaynak
11TH INTERNATIONAL MULTIDISCIPLINARY SCIENTIFIC GEOCONFERENCE (SGEM 2011), VOL I
WoS Q Değeri
N/A
Scopus Q Değeri
N/A
