Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Mohammad Poosti"'
Publikováno v:
پترولوژی, Vol 9, Iss 4, Pp 133-152 (2019)
In the western part of the Joupar Mountains, a set of Neogene basic rocks cover the felsic rocks. Volcanic rocks suite consisting of basalt- andesite- dacite and rhyolite. Main minerals in basaltic ricks consist of olivine, plagioclase, pyroxen and h
Externí odkaz:
https://doaj.org/article/20031a9e5129460faff4c8f7e0de4a3c
Publikováno v:
پترولوژی, Vol 9, Iss 3, Pp 173-192 (2018)
The Sarmeshk granitoid pluton is located in southeast of the Urumieh-Dokhtar magmatic zone in the Kerman province. Based on petrographic studies, the granitoid consist of three rock type of diorite, granodiorite and monzogranite. They are mainly comp
Externí odkaz:
https://doaj.org/article/a4624b14290846eb960fa78a5bdf19be
Publikováno v:
پترولوژی, Vol 8, Iss 32, Pp 1-20 (2018)
In the north of Kerman city, between Deh-Bazargan and Sarasiab 6 villages and along the Koohbanan fault, several lamprophyric dykes have been intruded the Shemshak, Bidu and Hodjedk Formations. The dykes show porphyry and glomeroporphyry textures and
Externí odkaz:
https://doaj.org/article/a744e441ff234452807be9bbc008b96b
Publikováno v:
Revista Brasileira de Paleontologia. 24:311-322
Fifteen conodont species and subspecies from the Negheleh section, Soh area, north of Esfahan represent early Eifelian to middle Givetian time interval. Five biozones: costatus to australis, kockelianus, ensensis to hemiansatus, timorensis and rhenan
Publikováno v:
Iranian Journal of Crystallography and Mineralogy. 27:123-134
Publikováno v:
International Geology Review. 62:1796-1814
The Sarduiyeh granitoid (SG) is intruded in the southeastern part of the Dehaj-Sarduiyeh volcano-sedimentary belt in the southeastern end of the Urumieh-Dokhtar Magmatic Arc (UDMA) in Iran. The med...
Publikováno v:
Energy Exploration & Exploitation. 29:109-128
The role of diagenesis in affecting (reduction or enhancement) reservoir quality in the Faraghan Formation in Darang #1 well was investigated. The Faraghan Formation is mainly composed of sandstone facies along with minor mudstone and siltstone and g