SODIUM SULFATE (GLAUBERITE-BLOEDITE) - HALITE ASSOCIATION in the TERTIARY (UPPER MIOSENE-PLIOCENE) KATRANDEDETEPE FORMATION, EREĞLİ-BOR BASIN, TURKEY

Gökhan KADINKIZ; Memet PEKGÖZ; Mustafa KARAKAŞ; Abdurrahman MURAT

doi:https://doi.org/10.19111/bulletinofmre.298685

Makale detayları

SODIUM SULFATE (GLAUBERITE-BLOEDITE) - HALITE ASSOCIATION in the TERTIARY (UPPER MIOSENE-PLIOCENE) KATRANDEDETEPE FORMATION, EREĞLİ-BOR BASIN, TURKEY

Yazarlar:

Gökhan KADINKIZ | Memet PEKGÖZ | Mustafa KARAKAŞ | Abdurrahman MURAT

Yayıncı:

Maden Tetkik Arama Genel Müdürlüğü

Ana Başlıklar:

Uygulamalı fizik

Dergi:

Bulletin of the Mineral Research and Exploration 2017 Vol.154 Issue 154, pp.135-156

Belge Tipi:

Makale

Yayın Tarihi:

4/2017

Belge Dili:

İngilizce

Document ID (Org No.):

2000520191

Sıklık:

Üç Yıllık

pISSN:

0026-4563

DOI:

https://doi.org/10.19111/bulletinofmre.298685

Özet:

 


This study covers the investigations
related to the glauberite-halite minerals detected in Neogene deposits of the
Ereğli-Bor Basin in the Central Anatolia. The basin consists of Paleozoic
basement rocks, the unconformably overlying Paleocene-Eocene-Oligocene marine sedimentary
and volcano-sedimentary rocks, and the Lower Miocene-Pliocene lake deposits at
the top, which unconformably overlie all underlying layers. In the study, core
drillings related to the determination of geological characteristics and
investigation of the mineral potential of buried salt deposits were carried out
in the Ereğli-Bor basin. As a result of drillings carried out,
glauberite-bloedite, halite and bituminous shale horizons, which possess
significant thickness and grade values, were cut for the first time in the
Konya-Ereğli-Bor basin. Glauberite minerals are observed in three different
structures as; 1- the Glauberite Mineral intercalated with High Graded, Bedded
Clays, 2- the Glauberite Mineral with Disseminated Rosette Type in Low Graded Clays
and 3- the Prismatic High Graded Glauberite Mineral intercalated with Halites.
Bloedite minerals are mostly observed with halite.It was detected that the economical evaporitic
formations in the Konya-Ereğli-Bor Basin had occurred within the Upper Miocene-Pliocene
Katrandedetepe Formation, which represents the playa-lake environment. 


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Makale detayları

SODIUM SULFATE (GLAUBERITE-BLOEDITE) - HALITE ASSOCIATION in the TERTIARY (UPPER MIOSENE-PLIOCENE) KATRANDEDETEPE FORMATION, EREĞLİ-BOR BASIN, TURKEY

Yazarlar: Gökhan KADINKIZ | Memet PEKGÖZ | Mustafa KARAKAŞ | Abdurrahman MURAT

Yayıncı: Maden Tetkik Arama Genel Müdürlüğü

Ana Başlıklar: Uygulamalı fizik

Dergi: Bulletin of the Mineral Research and Exploration 2017 Vol.154 Issue 154, pp.135-156

Belge Tipi: Makale

Yayın Tarihi: 4/2017

Belge Dili: İngilizce

Document ID (Org No.): 2000520191

Sıklık: Üç Yıllık

pISSN: 0026-4563

DOI: https://doi.org/10.19111/bulletinofmre.298685

Sayı

Yazarlar:

Gökhan KADINKIZ | Memet PEKGÖZ | Mustafa KARAKAŞ | Abdurrahman MURAT

Yayıncı:

Maden Tetkik Arama Genel Müdürlüğü

Ana Başlıklar:

Uygulamalı fizik

Dergi:

Bulletin of the Mineral Research and Exploration 2017 Vol.154 Issue 154, pp.135-156

Belge Tipi:

Makale

Yayın Tarihi:

4/2017

Belge Dili:

İngilizce

Document ID (Org No.):

2000520191

Sıklık:

Üç Yıllık

pISSN:

0026-4563

DOI:

https://doi.org/10.19111/bulletinofmre.298685