نتایج جستجو برای: mineral paragenesis

تعداد نتایج: 66715  

یوسف زاده, محمدحسین, سبزه ئی, مسیب,

The studied area is situated in southwestern Birjand (South Khorasan). Lithologic units which are studied contains part of the late Cretaceous coloured melange, Cretaceous and Paleogen flysh sediments, Neogen congolmerate and Tertiary volcanic rocks. The listwaenite of this area often appears along fault zone, boundary of units, bedding planes and schistiosity as yellow and brownish vein. ...

2014
Hazim Hrvatović

In this study two small, but genetically related iron carbonate deposits Mačje Jame and Vranjski Potok, south west of Busovača (MBSM), located in the pre-Devonian metamorphic complex were investigated in detail. Analyses of the main chemical components, trace elements, REE, isotope composition of C, O, S, 87Sr/86Sr ratio of rhyolite, plot of REE normalized to CI chondrites and a microscopic stu...

Journal: :مهندسی معدن 0
رضا قوامی ریابی دانشگاه صنعتی شاهرود میرمهدی سید رحیمی نیارق دانشگاه صنعتی شاهرود رضا خالوکاکایی دانشگاه صنعتی شاهرود محمد رضا هزاره سازمان زمین شناسی و اکتشافات معدنی کشور

the gold mineralization in kurdistan province of iran was classified as shear zone gold type by some of the researchers. in the current study, the geochemical samples collected from the secondary environment, stream sediments, at the sw of saqquez area were used to investigate the geochemical characteristics of the gold mineralized zones in this environment. the multi-variant statistical analys...

Journal: :Minerals 2022

The potential environmental impact of historical mining and ore processing on stream sediments water was studied in a small siderite iron deposit with diverse sulfide mineral paragenesis. main aim to characterize solid carriers potentially toxic elements (PTEs) mine waste, understand their fate fluvial systems. General mineralogy (X-ray powder diffraction) individual PTE (scanning electron micr...

Journal: :Contributions to Mineralogy and Petrology 2021

Abstract The major-element chemical composition of garnet provides valuable petrogenetic information, particularly in metamorphic rocks. When facing detrital garnet, information about the bulk-rock and mineral paragenesis initial garnet-bearing host-rock is absent. This prevents application thermo-barometric techniques calls for quantitative empirical approaches. Here we present a discriminatio...

Journal: :Frontiers in Earth Science 2023

This study presents rock slab and thin section reflection mapping, element mapping by Micro-XRF (μ-XRF) analysis, in situ cassiterite U-Pb laser ablation-inductively coupled plasma mass spectrometer (LA-ICP-MS) ages of the Xinlu Sn-Zn deposit, Nanling Sn-W belt, South China. The new results provided constraints on age processes Sn mineralization thus further discussed role Paleo-Pacific plate f...

Journal: :Open Journal of Applied Sciences 2023

The objective of the study was to characterize clays Lama depression in Benin. Macroscopic examination hand soundings, dynamic penetration test and stratigraphic correlation water borehole logs, as well scanning electron microscopy (SEM) combined with energy-dispersive X-ray microanalysis (EDX) method were made on compact or stratified clays. large grains are embedded a sintered matrix. texture...

قادری, مجید, رشیدنژاد عمران, نعمت‌اله , ویس‌کرمی, حدیث ,

Triassic (mostly volcanic-carbonate) and Jurassic (mainly shale and sandstone) rocks in west of Malayer were affected by a number of shear zone, folding, deformation and metamorphic events. Regional metamorphism in the area led to the formation of Triassic and Jurassic rocks such as phyllite, slate and crystalline carbonate which folded during deformational events. In the contact metamorphism e...

احمدی, علی, میرزایی راینی, رضوان , میرنژاد, حسن,

Mahour polymetal deposit located west of Nehbandan, east-central Iran, formed in hypabyssal acid rocks. Mineralization occurs along a three-km-long vein. Three zones have observed in the ore, downward: 1) leached zone marked by malachite, azurite, hematite, goethite and limonite, 2) supergene zone characterized by bornite, covellite, and chalcocite, and 3) Hypogene zone containing magnetite, ch...

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