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摘要:
To study petrography, microfacies, sedimentary environments and sequence stratigraphy of Asmari formation in central Fars, 4 stratigraphic sections have benn chosen and studied (Estahban, Shams-Abad, Sarvestan and Akbar-Abad Sections). Field and laboratories study recognized 16?carbonate microfacies and 2 clastic-carbanate facies. Study of microfacies, relative sea level?change and sequence stratigraphy evidences show these microfacies are deposited in carbonate ramp sedimentary environment in 5 facies belt zones: Open marine (A), Restricted (B), Shoal (C), Lagoon (D) and Tidal flat (E) during Oligomiocene. Petrography, microfacies analysis and sedimentary environment of Asmari formation shows this formation in study area consist of 3 depositional sequences. Lower sequence boundary of DS1 with Jahrum formation is erosional (disconformity) SB1. Lower and upper sequence boundary of DS2 is SB2. The upper sequence boundary of DS3 is SB1 and ended under the Razak clastic formation. In central Fars only lower part of Asmari is deposited and upper part of this formation have been eroded and disappeared.
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篇名 Petrography, Sedimentary Environments and Sequence Stratigraphy of Asmari Formation in Central Fars, Zagros, SW (Iran)
来源期刊 地质学期刊(英文) 学科 地球科学
关键词 PETROGRAPHY SEDIMENTARY Environment Sequence STRATIGRAPHY Asmari Formation ZAGROS Iran
年,卷(期) 2014,(12) 所属期刊栏目
研究方向 页码范围 665-679
页数 15页 分类号 P61
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研究主题发展历程
节点文献
PETROGRAPHY
SEDIMENTARY
Environment
Sequence
STRATIGRAPHY
Asmari
Formation
ZAGROS
Iran
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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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