THE Pb-Zn DEPOSITS IN THE SOUTHWEST OF TUTAK DAĞI (ŞEBİNKARAHİSAR-GİRESUN)

Ahmet ŞAŞMAZ; Ahmet SAĞIROĞLU

Makale detayları

THE Pb-Zn DEPOSITS IN THE SOUTHWEST OF TUTAK DAĞI (ŞEBİNKARAHİSAR-GİRESUN)

Yazarlar:

Ahmet ŞAŞMAZ | Ahmet SAĞIROĞLU

Yayıncı:

Maden Tetkik Arama Genel Müdürlüğü

Ana Başlıklar:

Uygulamalı fizik

Dergi:

Bulletin of the Mineral Research and Exploration 1994 Vol.116 Issue 116, pp.46-46

Belge Tipi:

Makale

Yayın Tarihi:

8/1994

Belge Dili:

İngilizce

Document ID (Org No.):

2000521268

Sıklık:

Üç Yıllık

pISSN:

0026-4563

Özet:

 


 The Pb-Zn cxe deposits of the area southwest of Tutak Mountain are situated in Eastern Black Sea Region, in the
southern parts of the Pontids Tectonic Unit and in roughly 20 km s northwest of Şebinkarahisar township The ore deposits are
studied in five sectors; this mineralizations are vein type The area is a part of Eastern Black Sea metallogenic province The
area is made up of volcanic, plutonic and sedimentary rocks of upper Cretaceous to Plio Quaternary These lithologies are as
follows; upper Cretaceous volcanics (dacites, andesites, pyrodastics) and carbonaceous sandstones, upper
Cretaceous-Paleogene granitoids, Eocene volcanics (andesites, basalts, trachiandesites and tuffites), Oligo-Miocene
gypsiferous senes (gypsium and mudstone), and Plio-Quaternary volcanies (andesite). The studied area has been subjected to
intense tectonic movements dunng upper Cretaceous and later Two main fault systems strike NE-SW and NW-SE The NE-SW
striking fault zone geherally mineralized and pre-Eocene aged and the NW-SE striking ones are post Eocene aged and not
mineralized. The mineralizations occur within a broad fault zone which strikes NE-SW This 250-300 m.s wide and 1.5-2 km s
long zone is faulted intensely, mineralized and altered The intensity of alteration changes vertically and honzontally The main
alterations in the studied area are siliafication, carbonatization, chlontization, argillization, epidotization and sencization These
alterations indicate a low to medium temperature of formation The ore minerals of the studied area are; sphalente, galena,
pyrite, chalcopynte, fahlore group minerals, calcocite-covellite and hematite Gangue minerals are quartz, calate, day minerals,
chtonte, hematite and bante

.

Makale detayları

THE Pb-Zn DEPOSITS IN THE SOUTHWEST OF TUTAK DAĞI (ŞEBİNKARAHİSAR-GİRESUN)

Yazarlar: Ahmet ŞAŞMAZ | Ahmet SAĞIROĞLU

Yayıncı: Maden Tetkik Arama Genel Müdürlüğü

Ana Başlıklar: Uygulamalı fizik

Dergi: Bulletin of the Mineral Research and Exploration 1994 Vol.116 Issue 116, pp.46-46

Belge Tipi: Makale

Yayın Tarihi: 8/1994

Belge Dili: İngilizce

Document ID (Org No.): 2000521268

Sıklık: Üç Yıllık

pISSN: 0026-4563

Sayı

Yazarlar:

Ahmet ŞAŞMAZ | Ahmet SAĞIROĞLU

Yayıncı:

Maden Tetkik Arama Genel Müdürlüğü

Ana Başlıklar:

Uygulamalı fizik

Dergi:

Bulletin of the Mineral Research and Exploration 1994 Vol.116 Issue 116, pp.46-46

Belge Tipi:

Makale

Yayın Tarihi:

8/1994

Belge Dili:

İngilizce

Document ID (Org No.):

2000521268

Sıklık:

Üç Yıllık

pISSN:

0026-4563