Search results for "Willemite"

showing 2 items of 2 documents

Distribution of trace elements in willemite from the Belgium non-sulphide deposits

2019

Samples of willemite (Zn2SiO4) mineralization from the historical non-sulphide Zn–Pb deposits of La Calamine (eastern Belgium) have been recovered from collections of the Geological Survey of Belgium. Textural and chemical analyses are used to evaluate the critical element distribution (Ge, In, Ga) and deportment. willemite occurs as a variety of types that continuously formed between the protore stage (sulphides) and the late supergene stage (carbonates and hydrated phases). Different types of willemite may be distinguished on the basis of their shape and zoning characteristics, supporting a polyphase non-sulphide mineralization after the protore stage. This is also marked by a significant…

Mineralization (geology)ChemistryGermanium05 social sciencesWillemiteGeochemistrychemistry.chemical_element[SDU.STU]Sciences of the Universe [physics]/Earth SciencesWillemiteZincengineering.materialHydrothermal circulationSupergeneNon-sulphide zinc depositsSphaleriteGeochemistry and PetrologyGalena[SDU]Sciences of the Universe [physics]0502 economics and businessCritical elementsengineering050211 marketingInductively coupled plasma050203 business & management[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/MineralogyEuropean Journal of Mineralogy
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Nature and origin of natural Zn clay minerals from the Bou Arhous Zn ore deposit: Evidence from electron microscopy (SEM-TEM) and stable isotope comp…

2016

International audience; Zn-clay minerals have been found in the non-sulfide deposit of Bou Arhous (High Atlas, Morocco). They occur as white or ochre clays embedding willemite (Zn2SiO4) and are commonly associated to red detrital clays in karstic cavities. Scanning Electron Microscopy (SEM), X-Ray Diffraction (XRD) and Transmission Electron Microscopy (TEM) with Energy Dispersive X-ray (EDX) analyses were combined in order to characterize the clay minerals and to determine the mechanism of their formation. XRD patterns on oriented and powdered clays and Fourier Transform Infrared (FTIR) spectroscopic analyses suggest that fraipontite is the major Zn clay phase (with some smectite interstrat…

Ore depositsScanning electron microscopeThin sectionWillemiteAnalytical chemistry[SDU.STU]Sciences of the Universe [physics]/Earth SciencesMineralogyStem010501 environmental sciencesengineering.material010502 geochemistry & geophysics01 natural sciencesGeochemistry and PetrologyClay mineral X-ray diffractionTexture (crystalline)FraipontiteDissolutionComputingMilieux_MISCELLANEOUSStable isotopes0105 earth and related environmental sciencesChemistryGeology[ SDU.STU ] Sciences of the Universe [physics]/Earth SciencesClay mineralogyZincFTIRTransmission electron microscopyTemengineeringClay minerals
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