Planktonic foraminiferal biostratigraphy of Upper Paleocene to Middle Eocene sequences in the Eastern Desert area, Egypt

Hiroshi Nishi; A. M.T. Elewa; K. Ishizaki

Planktonic foraminiferal biostratigraphy of Upper Paleocene to Middle Eocene sequences in the Eastern Desert area, Egypt

Hiroshi Nishi, A. M.T. Elewa, K. Ishizaki

学術資源研究公開センター・博物館

研究成果: Article › 査読

11 被引用数 (Scopus)

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Rocks exposed in this area comprise five lithological units, and can be divided into five planktonic foraminiferal biozones. The Esna Formation is assigned to the late Paleocene to latest early Eocene, and the Maghagha and Qarara Formations to the middle Eocene. The limestone-marl Maghagha Formation was deposited in the west, simultaneously with the sandstone-shale Qarara Formation in the east. -from Authors

本文言語	English
ページ（範囲）	521-552
ページ数	32
ジャーナル	Transactions & Proceedings - Palaeontological Society of Japan
巻	175
出版ステータス	Published - 1994 1月 1

ASJC Scopus subject areas

環境科学（全般）
地球惑星科学（全般）

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title = "Planktonic foraminiferal biostratigraphy of Upper Paleocene to Middle Eocene sequences in the Eastern Desert area, Egypt",

abstract = "Rocks exposed in this area comprise five lithological units, and can be divided into five planktonic foraminiferal biozones. The Esna Formation is assigned to the late Paleocene to latest early Eocene, and the Maghagha and Qarara Formations to the middle Eocene. The limestone-marl Maghagha Formation was deposited in the west, simultaneously with the sandstone-shale Qarara Formation in the east. -from Authors",

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T1 - Planktonic foraminiferal biostratigraphy of Upper Paleocene to Middle Eocene sequences in the Eastern Desert area, Egypt

AU - Nishi, Hiroshi

AU - Elewa, A. M.T.

AU - Ishizaki, K.

PY - 1994/1/1

Y1 - 1994/1/1

N2 - Rocks exposed in this area comprise five lithological units, and can be divided into five planktonic foraminiferal biozones. The Esna Formation is assigned to the late Paleocene to latest early Eocene, and the Maghagha and Qarara Formations to the middle Eocene. The limestone-marl Maghagha Formation was deposited in the west, simultaneously with the sandstone-shale Qarara Formation in the east. -from Authors

AB - Rocks exposed in this area comprise five lithological units, and can be divided into five planktonic foraminiferal biozones. The Esna Formation is assigned to the late Paleocene to latest early Eocene, and the Maghagha and Qarara Formations to the middle Eocene. The limestone-marl Maghagha Formation was deposited in the west, simultaneously with the sandstone-shale Qarara Formation in the east. -from Authors

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ER -

Planktonic foraminiferal biostratigraphy of Upper Paleocene to Middle Eocene sequences in the Eastern Desert area, Egypt

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