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摘要:
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.
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篇名 Genetic Relationship of Minerals and Carbonate Units of Stratigraphy Sequence in the Ahmadabad Deposit (NE of Bafq) Using Data Related to Rare Earth Elements
来源期刊 地质学期刊(英文) 学科 地球科学
关键词 Ahmadabad PB-ZN Ore DEPOSIT CARBONATE Rocks SEQUENCE Rare Earth Elements
年,卷(期) 2017,(7) 所属期刊栏目
研究方向 页码范围 1012-1021
页数 10页 分类号 P5
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Ahmadabad
PB-ZN
Ore
DEPOSIT
CARBONATE
Rocks
SEQUENCE
Rare
Earth
Elements
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研究来源
研究分支
研究去脉
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期刊影响力
地质学期刊(英文)
月刊
2161-7570
武汉市江夏区汤逊湖北路38号光谷总部空间
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585
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