Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Vahid Ahadnejad"'
Publikováno v:
Journal of Economic Geology, Vol 9, Iss 1, Pp 175-192 (2017)
Introduction The Jebale-Barez Plutonic Complex (JBPC) is composed of many intrusive bodies and is located in the southeastern province of Kerman on the longitude of the 57◦ 45 ' east to 58◦ 00' and Northern latitudes 28◦ 30' to 29◦ 00'. The
Externí odkaz:
https://doaj.org/article/4e24ee16ae384995bf6a0662a726584e
Autor:
Mohammad Reza Ghorbani, Mohammad Paydari, Parham Ahmadi, Albrecht von Quadt, Vahid Ahadnejad, John M. Cottle, Ian T. Graham, Jamshid Ahmadian, Ahmad Ahmadvand
Publikováno v:
International Journal of Earth Sciences. 112:1553-1575
Publikováno v:
The Journal of Gemmology. 38:329-347
Publikováno v:
Neues Jahrbuch für Mineralogie - Abhandlungen. 196:19-42
Biotite is the most frequent ferromagnesian phase in granitoids from the Malayer-Boroujerd Plutonic complex (MBPC), Zagros Orogen. The abundance of biotite decreases from granitoids towards dioritic intrusions, dioritic and gabbroic dykes to gabbroic
Publikováno v:
International Journal of Remote Sensing. 34:8803-8816
Hyperspectral images are widely employed for geological mapping because of their high spectral resolution. In this article, we develop the mixture-tuned matched filtering MTMF method, which can provide highly accurate mapping using the minimum ground
Publikováno v:
Arabian Journal of Geosciences. 9
The Uromia–Dokhtar Magmatic Arc (UDMA) is a northwest–southeast trending magmatic belt which is formed due to oblique subduction of Neotethys underneath Central Iran and dominantly comprises magmatic rocks. The Jebal-e-Barez Plutonic Complex (JBP
Publikováno v:
Natural Science. :91-105
The Boroujerd pluton (ca 175 Ma) was emplaced in the Sanandaj-Sirjan zone (SSZ) active margin of Central Iran consists of monzogranite, granodiorite, and quartz-diorite. Microstructural studies show a continuum from magmatic to (sub) mylonitic deform
Publikováno v:
Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 261:61-75
Publikováno v:
Geologica Carpathica. 62:171-180
The ammonium content in the Malayer igneous and metamorphic rocks (Sanandaj-Sirjan Zone, Western Iran)The ammonium (NH4+) contents of the Malayer area (Western Iran) have been determined by using the colorimetric method on 26 samples from igneous and