نتایج جستجو برای: garnet crystals

تعداد نتایج: 59350  

تقی‌پور, بتول, تقی‌پور, صدیقه, رهگشای, محمد, مکی‌زاده, محمدعلی ,

The Zaroo Cu-skarn is located NW of Yazd province, within the Cenozoic magmatic belt of Central Iran. The widespread rocks in the region are Eocene age volcanic with granitoids intrusives. The Cretaceous limestones in western parts of West Zaroo are hosted by skarn – marble mineralization. The skarns are distal type and are characterized by assemblage: Clinopyroxene, garnet, ilvaite, vezovianit...

2016
V. Lupei A. Lupei G. Boulon

The analysis of selective excitation and emission spectra of l'm3' in YAG and GGG laser systems is presented. The observed multisite structure is assigned to non-stoichiometric defects. Up to six centers are separated, with complex spectra connected with lowering of the local symmetry.

Journal: :Journal of Mineralogical and Petrological Sciences 2023

Needle-shaped rutile inclusions occur in garnet within the quartz-eclogite at Mt. Gongen Sanbagawa belt, central Shikoku. They are approximately 5–25 µm along long axis and typically oriented three directions, each intersecting 120°. This indicates that needle-shaped is a lamella exsolved from garnet. Garnet with needle-rutile restricted to quartz-poor domain of quartz eclogite sample, which co...

مجرد, منیر , محامد, امیر,

Eslamlu contact aureole, which is located at northern Oshnavieh Township, contains metapelites, calcsilicates and calcite-dolomite marbles. Some Cld, Grt, Crd, and porphyroblasts together with Sil, Hc and graphite crystals are existing at the metapelites. The most significant feature of Eslamlu aureole is its index informative reaction textures of metapelites through which metamorphic reactions...

2003
L. F. DOBRZHINETSKAYA H. W. GREEN K. N. BOZHILOV R. M. DICKERSON

Nanometric solid inclusions in diamond incorporated in garnet and zircon from felsic gneiss of the Kokchetav massif, Kazakhstan, have been examined utilizing electron microscopy and focused ion beam techniques. Host garnet and zircon contain numerous pockets of multiple inclusions, which consist of 1–3 diamond crystals intergrown with quartz, phengite, phlogopite, albite, K-feldspar, rutile, ap...

Journal: :زمین شناسی اقتصادی 0
میر علی اصغر مختاری محمد ابراهیمی محمد رضا قربانی

introduction the avan cu-fe skarn is located at the southern margin of qaradagh batholith, about 60 km north of tabriz. the skarn-type metasomatic alteration is the result of qaradagh batholith intrusion into the upper cretaceous impure carbonates. the studied area belongs to the central iranian structural zone. in regional scale, the studied area is a part of the zangezour mineralization zone ...

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