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Mineral chemistry, paragenesis and geochronological studies of the Hormuz Formation diabase rocks in the salt domes of sothern Iran, Hormozgan Province

Müellif Iranian journal of crystallography and mineralogy
Materyal türü Basma eser
Dil Farsça
Tarih 2018
Yüzyıl 21. yüzyıl
Kurum Internet Archive
Kaynak Internet Archive
Not The studied diabase rocks of the Hormuz Formation have undergone a variety of secondary processes and greenschist facies to amphibolite facies metamorphism. These rocks are metasomatized due to the effect of infiltrating metasomatism and hydrothermal alteration and are metamorphed due to CO 2 -rich
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Iranian journal of crystallography and mineralogy, Mineral chemistry, paragenesis and geochronological studies of the Hormuz Formation diabase rocks in the salt domes of sothern Iran, Hormozgan Province, 2018, Internet Archive, https://archive.org/details/8_20250409_202504.

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