DISCUSSION ON THE ORIGIN OF OTLUKİLİSE IRON DEPOSIT GÜRÜN-SİVAS

Dönmez ÇİFTÇİ; Taner ÜNLÜ; İ. Sönmez SAYILI

Makale detayları

DISCUSSION ON THE ORIGIN OF OTLUKİLİSE IRON DEPOSIT GÜRÜN-SİVAS

Yazarlar:

Dönmez ÇİFTÇİ | Taner ÜNLÜ | İ. Sönmez SAYILI

Yayıncı:

Maden Tetkik Arama Genel Müdürlüğü

Ana Başlıklar:

Uygulamalı fizik

Dergi:

Bulletin of the Mineral Research and Exploration 1996 Vol.118 Issue 118, pp.25-50

Belge Tipi:

Makale

Yayın Tarihi:

10/1996

Belge Dili:

İngilizce

Document ID (Org No.):

2000521187

Sıklık:

Üç Yıllık

pISSN:

0026-4563

Özet:

 


 In this study, the geological aspects of Otlukilise iron deposit near Gürün (Sivas, Turkey) is investigated and possible
mechanicms responsible for the formation of that deposit are discussed.
Otlukilise iron occurrences are located in volcanosedimentary levels in Yanıktepe and Akdere formations which are age of
Upper Cretaceous and Paleocene, respectively.
The occurrence of Otlukilise iron formations is belived to have taken place as enrichments by secondary processes from
siderite ores volcanosedimentary origin in relation with volcanic intercalations. Studies carried out on iron rich massive ores
indicate an old formation in a sedimentary basin that represented by cumulative supplements of iron and associated elements
which are directly on indirectly leached from serpentinites by submarine volcanites spreading out into an environment of carbonate
deposition and hydrothermal exhalative fluxes and associated silicate phases formed by intensive silica rich fluids of
hydrothermal origin and sulphide phases resulted from reactions of seewater and the same submarine volcanites.
Sequential conjugateness observed especially among quartz and siderite, clay and/or clay bearing siderite layers in iron
poor conglomerate breccia ore samples and estimations realized by certain mathematical rules indicate a sedimentary relationship
prior to deformation. Both massive ores and fragments are deposited by the processes during formation of an ore horizon
intercalated by clay and quartz rich levels and/or just after the movements at the bottom of the basin. Thus, Otlukilise iron
deposits represent an other sample of Lahn-Dill type syn-sedimentary volcanogenic or exhalative-sedimentary type ore formation
as Deveci Iron Deposits (Hekimhan-Malatya, Turkey) do. 

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Makale detayları

DISCUSSION ON THE ORIGIN OF OTLUKİLİSE IRON DEPOSIT GÜRÜN-SİVAS

Yazarlar: Dönmez ÇİFTÇİ | Taner ÜNLÜ | İ. Sönmez SAYILI

Yayıncı: Maden Tetkik Arama Genel Müdürlüğü

Ana Başlıklar: Uygulamalı fizik

Dergi: Bulletin of the Mineral Research and Exploration 1996 Vol.118 Issue 118, pp.25-50

Belge Tipi: Makale

Yayın Tarihi: 10/1996

Belge Dili: İngilizce

Document ID (Org No.): 2000521187

Sıklık: Üç Yıllık

pISSN: 0026-4563

Sayı

Yazarlar:

Dönmez ÇİFTÇİ | Taner ÜNLÜ | İ. Sönmez SAYILI

Yayıncı:

Maden Tetkik Arama Genel Müdürlüğü

Ana Başlıklar:

Uygulamalı fizik

Dergi:

Bulletin of the Mineral Research and Exploration 1996 Vol.118 Issue 118, pp.25-50

Belge Tipi:

Makale

Yayın Tarihi:

10/1996

Belge Dili:

İngilizce

Document ID (Org No.):

2000521187

Sıklık:

Üç Yıllık

pISSN:

0026-4563