Kerogen as a Source of Sulfur in MVT Deposits

2015 ◽  
Vol 110 (3) ◽  
pp. 837-840 ◽  
Author(s):  
G. M. Anderson
Keyword(s):  
2020 ◽  
Author(s):  
Ali Erdem Bakkalbasi ◽  
Hatice Nur Bayram ◽  
Mustafa Kumral ◽  
Ali Tugcan Unluer

<p><strong>Geochemical significance and Formation of  Suçatı Pb-Zn Deposits – Eastern Taurides</strong></p><p>Hatice Nur Bayram<sup>(1)*</sup>, Ali Erdem Bakkalbaşı <sup>(1)*</sup>, Mustafa Kumral<sup>(1)</sup>, Ali Tuğcan Ünlüer<sup>(1)</sup></p><p><sup>(1)</sup>Istanbul Technical University, Department of Geological Engineering, Istanbul/Turkey</p><p>(*E-mail: [email protected])</p><p> </p><p>The Middle Tauride Orogenic Belt is a productive enviroment in terms of Pb-Zn ore deposits, mostly associated with Permian aged dolomitized, shallow marine platform type carbonate rocks. There have been many studies on the origin of the ore deposits in the region, there are two important approaches that stand out for the formation of the ore deposits: the first theory is hydrothermal deposits with magmatic origin, and the other theory is Missisippi Valley-type (MVT) deposits related with the carbonate rocks commonly found in the region. Field studies at the Suçatı (Kayseri – Yahyalı, Central Anatolia, Turkey, East of Aladağlar extension of the Taurides) ore district in the Aladağ geologic unit indicate that the deposits in the region are associated with Paleo-Tethys limestones, fossiliferous limestones and dolomitic limestones. Mineralization is related to Lower Permian aged carbonate rocks include primary mineralization ore minerals as galena, sphalerite, smithsonite and goethite and as a product of hydrothermal activity, calcite mineral filled within fractures and cracks represents gangue minerals. As a result of geochemical analysis of the samples collected from the ore zones, PbO values range between 25.93% - 0.012%, ZnO values range between 51.01% - 0.042%, Fe<sub>2</sub>O<sub>3</sub> values range between 42.81% - 10.21%. In conclusion hydrothermal activities closely related with compressional and extentional tectonic regimes took place in multiphase mineralization.</p><p> </p><p><strong>Keywords:</strong> Pb-Zn Deposits, MVT, Taurides, Yahyalı</p>


2014 ◽  
Vol 88 (s2) ◽  
pp. 219-220 ◽  
Author(s):  
Yudong WU ◽  
Zongqi WANG ◽  
Jinhai LUO ◽  
Quanren YAN ◽  
Yinli ZHANG

Minerals ◽  
2019 ◽  
Vol 9 (3) ◽  
pp. 142
Author(s):  
Eduardo González-Partida ◽  
Antoni Camprubí ◽  
Alejandro Carrillo-Chávez ◽  
Erik Díaz-Carreño ◽  
Luis González-Ruiz ◽  
...  

The authors make the following corrections to this paper [...]


2009 ◽  
Vol 101 (1) ◽  
pp. 40
Author(s):  
Francisco González-Sánchez ◽  
Antoni Camprubí ◽  
Eduardo González-Partida ◽  
Carles Canet ◽  
Antonin Richard ◽  
...  

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