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摘要:
The Fahliyan Formation is a carbonate sequence of Lower Cretaceous (Berriasian-Hauterivian) in age and was deposited in the Zagros sedimentary basin. This formation is a part of Khami Group and is a reservoir rock in Zagros Basin. This formation was investigated by a detailed petrographic analysis in order to clarify the depositional facies and sedimentary environment in the Kuh-e-Gadvan in Fars Province. Petrographic studies led to the recognition of nine microfacies that were deposited in four facies belts: tidal flat, lagoon, and barrier and shallow open-marine. An absence of turbidite deposits, reefal facies, and gradual facies changes indicate that the Fahliyan Formation was deposited on a carbonate ramp.
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篇名 Microfacies and Sedimentary Environments of the Fahliyan Formation from the Southwest of Iran (Shiraz, Zagros)
来源期刊 地质学期刊(英文) 学科 地球科学
关键词 MICROFACIES SEDIMENTARY Environments Faliyan SHIRAZ ZAGROS
年,卷(期) 2013,(2) 所属期刊栏目
研究方向 页码范围 49-53
页数 5页 分类号 P61
字数 语种
DOI
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研究主题发展历程
节点文献
MICROFACIES
SEDIMENTARY
Environments
Faliyan
SHIRAZ
ZAGROS
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研究分支
研究去脉
引文网络交叉学科
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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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0
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