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Journals / Maden Tetkik ve Arama Dergisi / 1990 / Cilt: 111 - Sayı: 111

ROCK AND CLAY MINERALOGY OF THE UPPER CRETACEOUS-TERTIARY SEDIMENTARY SEQUENCE AROUND BURDUR LAKE

Emel BAYHAN
Hüseyin YALÇIN
Pages
52–52
Publication Date
1990-04-01
DOI
—
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AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

Rock and clay mineralogy of the units have been studied and their mode of occurrence discussed.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:Rocks and clay mineralogy of the Upper Cretaceous marine and Neogene shallow water units around Burdur lake have been studied.
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Key Findings & Data:Characteristic minerals of the Upper Cretaceous are dolomite and corrensite, Paleocene-Lower Eocene is smectite, Neogene are aragonite, analcime and smectite.
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Conclusion & Impact:Rock and clay mineralogy of the units have been studied and their mode of occurrence discussed.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters

Abstract

Rocks and clay mineralogy of the Upper Cretaceous marine and Neogene shallow water units around Burdur lake have been studied. Characteristic minerals of the Upper Cretaceous are dolomite and corrensite, Paleocene-Lower Eocene is smectite, Neogene are aragonite, analcime and smectite. Calcite, quartz, feldspar, illite and chlorite are commonly found in all these units. It has been shown that rock units of different age and environment differ from one another in respect to their rock and clay mineralogy. Rock and clay mineralogy of the units have been studied and their mode of occurrence discussed.

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Cite This Article

BAYHAN, E., YALÇIN, H. (1990). ROCK AND CLAY MINERALOGY OF THE UPPER CRETACEOUS-TERTIARY SEDIMENTARY SEQUENCE AROUND BURDUR LAKE. Maden Tetkik ve Arama Dergisi, Cilt: 111 - Sayı: 111, 52–52. https://ajindex.com/articles/54339

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