نتایج جستجو برای: forumad ophiolite

تعداد نتایج: 1055  

احمد, احمدحسن, ترابی, قدرت, آرایی, شوجی , سبزه‌یی, مسیب , شیراساکا, میکی ,

In the upper Proterozoic Anarak ophiolite, the marbles are present and havr excellent exposures in different areas. Their best exposure is in southern slope of Chah-Gorbeh mountain (Chah-Mahdi valley). In the field, marbles have massive and dike like exposures. Petrographic studies and geochemistry of minerals show that marbles consist of carbonate (calcite), garnet (andradite), clinopyroxene (...

Journal: :زمین شناسی اقتصادی 0
محمد حسین زرین کوب سون لین چانگ سید سعید محمدی محمد مهدی خطیب

bibi maryam granitoid body with about 5 km2 has intruded into ophiolite mélange complex in sistan suture zone, in east of iran. thermal effects of this body on the host rocks show that this activity occurred after emplacement of ophiolite mélange. this intrusive body with general northwest – southeast trend is mainly tonalite-quartz diorite but there is a minor unit as dykes of granodiorite in ...

مرادپور, علی, زارعی سهامیه, رضا ,

Ophiolites of the Zagros orogenic belt are part of the Tethys ophiolites, because of their geographical locations and link the Middle East ophiolites and other Asian ophiolites (e.g. Pakistani and Tibetan) to the Mediterranean ophiolites (e.g. Troodos , Greek and East European). The nature of the Harsin- Sahneh ophiolite (Kermanshah) traditionally identified as one of the Mesozoic southern bran...

Journal: :journal of tethys 0

the serpentinization of the harzburgitic mantle section of the bou azzer neoproterozoic ophiolite is studied by field mapping, structural observations, optical micrography, sem and x-ray diffractometry, and relationships with co, ni, cr and sulphides minerals are discussed. serpentinization occurred in two major steps with, i) intra-oceanic pseudomorphic serpentinization materialized by the iso...

2013
I. PANAGIOTAKIS D. DERMATAS C. VATSERIS M. CHRYSOCHOOU N. PAPASIOPI A. XENIDIS E. THEOLOGOU T. MPOURAS L. SAKELLARIOU

Chromium (Cr) is a heavy metal that naturally occurs in the Earth’s crust, and can be found in groundwater in either the trivalent, Cr(III), or in the hexavalent, Cr(VI), form. While Cr(III) is considered an essential trace element for the human body, Cr(VI) is potentially dangerous for human health although the type and intensity of the effect are still being investigated. The widespread use o...

Journal: :Journal of Geography (Chigaku Zasshi) 1989

Journal: :Bulletin of the Geological Society of Greece 2007

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