نتایج جستجو برای: tuffs

تعداد نتایج: 354  

مهوری, رضوان, مکی‌زاده, محمدعلی, نقره‌ئیان, موسی,

Kalchoyeh copper deposit is located about 110 km east of Isfahan, in Central Iran, Urumieh- Bazman volcanoplutonic belt. Host rocks of this deposit are Eocene volcanic rocks and tuffs which are pyroxene andesitic lava and sandy and lithic tuffs. Sandy tuffs are the main host rocks of the deposit. Ore mineralization is taken place as veins and veinlets and quartz is the main gangue mineral. Hypo...

2013
E. Yasar Tuff Stone Mustafa Pasa

In the study, availability of tuffs around Erkilet (Kayseri), Kayseri and Mustafa Pasa (Nevsehir), Göreme (Nevsehir) and Nevsehir for using in many stages of construction materials, especially in blocks, shaped production, pavement, sideways, bordure and in landscape architecture was examined and samples were collected. For this purpose, standards experimental samples size of tuffs were prepare...

1981
David L. Bish

The detailed mineralogy of the Bullfrog and Tram Members of the Crater Flat Tuff from drill hole USW-G1 has been examined, primarily to characterize fully the amounts and types of clay minerals in the tuffs and the possible effects clay minerals have on rock properties. Results of bulk sample x-ray diffraction analyses agree closely with previous determinations, although slightly higher clay mi...

Journal: :Geological Magazine 1964

Journal: Geopersia 2011
Ali Abedini Ali Asghar Calagari Masoomeh Akbari

Mehredjan bentonite deposit is located ~33 km southeast of Khoor in Isfehan province. It includes 15 discrete outcrops and occurs as layered and massive forms within a volcano-clastic sequence. Bentonitization process was accompanied with development of minerals such as montmorillonite, quartz, cristobalite, calcite, kaolinite, halite, albite, orthoclase, and muscovite. The collected field and ...

توکلی, سمیه, بدیعی, علیرضا , برقی, محمدعلی , طوطی, فرامرز ,

In order to investigate the alteration products of rhyolitic tuffs under alkaline hydrothermal condition, samples of acidic pyroclastic rocks from Darabad area (N-E Tehran) were selected. Rock samples were examined under petrographic microscope, X-Ray powder diffraction, X-Ray Fluorescence and were eventually powdered and mixed with Na+ and K+ bearing solutions in hydrothermal autoclaves. The e...

Journal: :JORDANIAN JOURNAL OF ENGINEERING AND CHEMICAL INDUSTRIES (JJECI) 2019

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