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Gilg, H.A. and Boni, M. (2004) stable Isotope Composition of on Zn and Pb Carbonates; Their Role in Exploration of Non-Sulphide Ores. In: Boni, M., Ed., Publication-Geology Department and Extension Service, University of Western Australia, Australia, University of Western Australia, Geology Department and Extension Service: Perth, Eest. Aust., Australia, 361-365.

has been cited by the following article:

• TITLE: Genetic Relationship of Minerals and Carbonate Units of Stratigraphy Sequence in the Ahmadabad Deposit (NE of Bafq) Using Data Related to Rare Earth Elements

  AUTHORS: Sara Amani Lari, Iraj Rassa, Ali Amiri

  KEYWORDS: Ahmadabad Pb-Zn Ore Deposit, Carbonate Rocks Sequence, Rare Earth Elements

  JOURNAL NAME: Open Journal of Geology, Vol.7 No.7, July 24, 2017

  ABSTRACT: Ahmadabad Pb-Zn ore deposit is located in the mineral area of Bahabad in Central Iran Zone. This ore deposit like other metallogenic areas in Bahabad is found in Triassic carbonate rocks. Carbonate rocks in Shotori formation have the highest frequency in the regional sequence stratigraphy. This formation is composed of TRSh1, TRSh2, TRSh3 and TRSh4 units. The TRSh3 unit hosts minerals in ore deposit Ahmadabad. Microcrystalline particles are the main constituent of these rocks. The most important minerals in this ore deposit include calamine Celestine, Cerussite and Wulfenite. The comparison of normalized ore patterns and carbonate sequence indicates that they have a specified genetic relationship. Here the TRSh2 unit is more similar to minerals.