Résumé
L’étude pétrologique du massif volcanique plio-quaternaire du Kouh-e-Shahsavaran Iran méridional) permet de mettre en évidence l’existence d’une serie calco-alcaline (41 analyses chimiques d’éléments majeurs) dans laquelle les andésites predominent sur les autres laves. A partir de ce résultat et en tenant compte des données structurales, les auteurs discutent la présence d’une zone de subduction au Nord du Golfe d’Oman, entre les plaques arabique, eurasienne et indienne. Le Makran pourrait alors correspondie à une losse émergée.
Abstract
Kouth-e-Shasavaran massif in South Iran (Baloutchistan) consists of Pliocene and Quaternary cale-alkaline lavas. Fourty one new chemical analysis have been carried out to identify the volcanic rock series. Andesites are more abundant than basic thigh alumina basalts) and acid lavas (dacites and rhyodacites). This volcanic area is probably connected with a subduction zone located on the North of Oman Gulf, between the arabic, indian and eurasian plates. In this respect, Makran range may be inerpreted as an emerged trench.
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Contribution C.G.G. n. 187.
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Girod, M., Conrad, G. Les formations volcaniques récentes du Sud de l’Iran (Kouh-e-Shahsavaran): données pétrologiques préliminaires; implications structurales. Bull Volcanol 39, 495–511 (1975). https://doi.org/10.1007/BF02596972
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DOI: https://doi.org/10.1007/BF02596972