Highly metasomatised mantle as the main sources of Paleogene volcanism in the Saveh area, central Iran

Nouri, Fatemeh; Azizi, Hossein; Asahara, Yoshihiro; Stern, Robert

doi:10.14862/geochemproc.67.0_195

2020年度日本地球化学会第67回年会講演要旨集

DOI https://doi.org/10.14862/geochemproc.67.0_195

会議情報

主催: 日本地球化学会年会要旨集

会議名: 2020年度日本地球化学会第67回年会講演要旨集

回次: 67

開催日: 2020/11/12 - 2020/11/26

S3　考古と文化財の地球化学

Highly metasomatised mantle as the main sources of Paleogene volcanism in the Saveh area, central Iran

*Nouri, Fatemeh, Azizi, Hossein, Asahara, Yoshihiro, Stern, Robert

著者情報

キーワード: イラン, ザグロス造山帯, 火成活動, マントル, アラビア-イランプレート衝突

会議録・要旨集フリー

p. 195-

詳細

抄録

The Zagros orogenic belt of Iran consists of three parallel tectonic zones: Zagros fold-and-thrust belt, Sanandaj-Sirjan zone, and Urumieh-Dokhtar magmatic assemblage (UDMA). The UDMA includes igneous rocks from calc alkaline to alkaline and shoshonitic series. The aim of this study is to understand the petrogenesis of the Paleogene Saveh volcanic rocks in the UDMA by petrological, chemical and Sr-Nd isotopic analysis.

責任著者(Corresponding author)

J-STAGEへの登録はこちら（無料）