Akçataş granite is located in the northwest of Nevşehir. Granites, orthodase granites, orthoclase granite with oligoclase, granodiorites,
quartzdiorites, diorite (albitized), syenites, monzonites, quartzmonzonite, monzodiorite and altered plutonic rocks (granites and/
or orthoclase granites) are identified in pluton. The enclaves are sparsely observed in granites and granodiorites. Abyssal rocks are determined
as granite aplite, granite porphyre, diorite porphyrite (albitized). Field and microscobik studies show that magma has become differentiated
twice, has generally assimilated the pieces of adjacent sedimentary rocks, intruded not deeper than the top level of the mesozone,
genesis of enclaves are identical with plutonic rocks and hydrothermal stage was effective.
Birincil Dil | İngilizce |
---|---|
Konular | Mühendislik |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 1 Mayıs 1991 |
Yayımlandığı Sayı | Yıl 1991 Cilt: 112 Sayı: 112 |
Copyright and Licence
The Bulletin of Mineral Research and Exploration keeps the Law on Intellectual and Artistic Works No: 5846. The Bulletin of Mineral Research and Exploration publishes the articles under the terms of “Creatice Common Attribution-NonCommercial-NoDerivs (CC-BY-NC-ND 4.0)” licence which allows to others to download your works and share them with others as long as they credit you, but they can’t change them in any way or use them commercially.
For further details;
https://creativecommons.org/licenses/?lang=en