『徳島大学 教育・研究者情報データベース (EDB)』---[学外] /
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EID=314070EID:314070, Map:0, LastModified:2016年9月29日(木) 15:39:39, Operator:[石田 啓祐], Avail:TRUE, Censor:承認済, Owner:[石田 啓祐], Read:継承, Write:継承, Delete:継承.
種別 (必須): 学術論文 (審査論文) [継承]
言語 (必須): 英語 [継承]
招待 (推奨):
審査 (推奨): Peer Review [継承]
カテゴリ (推奨): 研究 [継承]
共著種別 (推奨):
学究種別 (推奨):
組織 (推奨):
著者 (必須): 1. (英) Shigeyuki Suzuki (日) (読)
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[継承]
2. (英) Rolando E. Peña (日) (読)
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3. (英) Tomas A. Tam (日) (読)
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[継承]
4. (英) Graciano P. Yumul, Jr. (日) (読)
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5. (英) Carla B. Dimalanta (日) (読)
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[継承]
6. (英) Mayumi Usui (日) (読)
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7.石田 啓祐
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題名 (必須): (英) Development of the Philippine Mobile Belt in northern Luzon from Eocene to Pliocene  (日)    [継承]
副題 (任意):
要約 (任意): (英) The origin of the Philippine Archipelago is characterized by the combination of the oceanic Philippine Mobile Belt (PMB) and the Palawan Continental Block (PCB). This paper is focused on the geologic evolu- tion of the PMB in northern Luzon from Eocene to Pliocene. The study areas (northern Luzon) are situated in the central part of the PMB which is occupied by its typical components made up of a pre-Paleocene ophiolitic complex, Eocene successions, Eocene to Oligocene igneous complex and late Oligocene to Pliocene successions. Facies analysis of the middle Eocene and late Oligocene to early Pliocene successions was carried out to understand the depositional environment of their basins. Modal sandstone com- positions, which reflect the basement geology of the source area, were analyzed. Major element geochemistry of sediments was considered to reconstruct the tectonic settings. The following brief history of the PMB is deduced. During the middle Eocene, the PMB was covered by mafic volcanic rocks and was a primitive island arc. In late Eocene to late Oligocene time, the intermediate igneous complex was added to the mafic PMB crust. By late Oligocene to early Miocene time, the PMB had evolved into a volcanic island arc setting. Contributions from alkalic rocks are detected from the rock fragments in the sandstones and chemical composition of the Zigzag Formation. During the middle Miocene to Pliocene, the tectonic setting of the PMB remained as a mafic volcanic island arc.  (日)    [継承]
キーワード (推奨):
発行所 (推奨): (英) Elsevier (日) (読) [継承]
誌名 (必須): Journal of Asian Earth Sciences ([Elsevier])
(pISSN: 1367-9120, eISSN: 1878-5786)

ISSN (任意): 1367-9120
ISSN: 1367-9120 (pISSN: 1367-9120, eISSN: 1878-5786)
Title: Journal of Asian earth sciences
Title(ISO): J Asian Earth Sci
Publisher: Elsevier Ltd
 (NLM Catalog  (Scopus  (CrossRef (Scopus information is found. [need login])
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(必須): Special issue "Crust Mantle Evolution" [継承]
(必須): (published online) [継承]
(必須): in press [継承]
都市 (任意): (英) Oxford(United Kingdom) (日) (読) [継承]
年月日 (必須): 西暦 2016年 8月 22日 (平成 28年 8月 22日) [継承]
URL (任意): http://dx.doi.org/10.1016/j.jseaes.2016.08.018 [継承]
DOI (任意): 10.1016/j.jseaes.2016.08.018    (→Scopusで検索) [継承]
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標準的な表示

和文冊子 ● Suzuki Shigeyuki, Peña E. Rolando, Tam A. Tomas, Jr. P. Yumul Graciano, Dimalanta B. Carla, Usui Mayumi and Keisuke Ishida : Development of the Philippine Mobile Belt in northern Luzon from Eocene to Pliocene, Journal of Asian Earth Sciences, Special issue "Crust Mantle Evolution", (published online), in-press, 2016.
欧文冊子 ● Suzuki Shigeyuki, Peña E. Rolando, Tam A. Tomas, Jr. P. Yumul Graciano, Dimalanta B. Carla, Usui Mayumi and Keisuke Ishida : Development of the Philippine Mobile Belt in northern Luzon from Eocene to Pliocene, Journal of Asian Earth Sciences, Special issue "Crust Mantle Evolution", (published online), in-press, 2016.

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