Details
| Originalsprache | Englisch |
|---|---|
| Seiten (von - bis) | 227-240 |
| Seitenumfang | 14 |
| Fachzeitschrift | Neues Jahrbuch fur Geologie und Palaontologie - Abhandlungen |
| Jahrgang | 262 |
| Ausgabenummer | 2 |
| Frühes Online-Datum | Sept. 2011 |
| Publikationsstatus | Veröffentlicht - 1 Nov. 2011 |
Abstract
Paleozoic of Jandaq and Posht-e-Badam ophiolites and Mesozoic ophiolitic mélanges of Nain and Ashin are located in the western part of the Central East Iranian Microcontinent. They are metamorphic relicts within the amphibolite faciès of Paleo-Tethys and Neotethys Oceans. Petrological and geochemical studies of these Paleozoic and Mesozoic ophiolites suggest that they include oceanic basic dykes, pillow and massive lavas formed during mid-oceanic rifting processes. Parental basic rocks from Paleozoic ophiolites of Jandaq and Posht-e-Badam have tholeiitic to alkaline affinities. They are supposed to have been generated by lower partial melting of a relatively enriched mantle peridotite. Parental basic rocks from Mesozoic ophiolites have typical N-MORB affinity and were generated by partial melting of a depleted mantle source.
ASJC Scopus Sachgebiete
- Erdkunde und Planetologie (insg.)
- Paläontologie
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in: Neues Jahrbuch fur Geologie und Palaontologie - Abhandlungen, Jahrgang 262, Nr. 2, 01.11.2011, S. 227-240.
Publikation: Beitrag in Fachzeitschrift › Artikel › Forschung › Peer-Review
}
TY - JOUR
T1 - Paleozoic and Mesozoic ophiolites of Central Iran
T2 - Amphibolites from Jandaq, Posht-e-Badam, Nain and Ashin ophiolites
AU - Torabi, Ghodrat
AU - Shirdashtzadeh, Nargess
AU - Arai, Shoji
AU - Koepke, Jürgen
PY - 2011/11/1
Y1 - 2011/11/1
N2 - Paleozoic of Jandaq and Posht-e-Badam ophiolites and Mesozoic ophiolitic mélanges of Nain and Ashin are located in the western part of the Central East Iranian Microcontinent. They are metamorphic relicts within the amphibolite faciès of Paleo-Tethys and Neotethys Oceans. Petrological and geochemical studies of these Paleozoic and Mesozoic ophiolites suggest that they include oceanic basic dykes, pillow and massive lavas formed during mid-oceanic rifting processes. Parental basic rocks from Paleozoic ophiolites of Jandaq and Posht-e-Badam have tholeiitic to alkaline affinities. They are supposed to have been generated by lower partial melting of a relatively enriched mantle peridotite. Parental basic rocks from Mesozoic ophiolites have typical N-MORB affinity and were generated by partial melting of a depleted mantle source.
AB - Paleozoic of Jandaq and Posht-e-Badam ophiolites and Mesozoic ophiolitic mélanges of Nain and Ashin are located in the western part of the Central East Iranian Microcontinent. They are metamorphic relicts within the amphibolite faciès of Paleo-Tethys and Neotethys Oceans. Petrological and geochemical studies of these Paleozoic and Mesozoic ophiolites suggest that they include oceanic basic dykes, pillow and massive lavas formed during mid-oceanic rifting processes. Parental basic rocks from Paleozoic ophiolites of Jandaq and Posht-e-Badam have tholeiitic to alkaline affinities. They are supposed to have been generated by lower partial melting of a relatively enriched mantle peridotite. Parental basic rocks from Mesozoic ophiolites have typical N-MORB affinity and were generated by partial melting of a depleted mantle source.
KW - Amphibolite
KW - Central iran
KW - Mesozoic
KW - Ophiolite
KW - Paleozoic
UR - http://www.scopus.com/inward/record.url?scp=82355169194&partnerID=8YFLogxK
U2 - 10.1127/0077-7749/2011/0194
DO - 10.1127/0077-7749/2011/0194
M3 - Article
AN - SCOPUS:82355169194
VL - 262
SP - 227
EP - 240
JO - Neues Jahrbuch fur Geologie und Palaontologie - Abhandlungen
JF - Neues Jahrbuch fur Geologie und Palaontologie - Abhandlungen
SN - 0077-7749
IS - 2
ER -