E. Crespo-Feo

ORCID: 0000-0003-2173-9325
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About
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Research Areas
  • Geological and Geochemical Analysis
  • Luminescence Properties of Advanced Materials
  • Glass properties and applications
  • Building materials and conservation
  • Geological and Geophysical Studies Worldwide
  • Mineralogy and Gemology Studies
  • Crystal Structures and Properties
  • Mine drainage and remediation techniques
  • Clay minerals and soil interactions
  • earthquake and tectonic studies
  • Heavy metals in environment
  • Graphite, nuclear technology, radiation studies
  • Nuclear materials and radiation effects
  • Geochemistry and Geologic Mapping
  • Conservation Techniques and Studies
  • Geological and Geophysical Studies
  • Archaeological and Geological Studies
  • Concrete and Cement Materials Research
  • Planetary Science and Exploration
  • High-pressure geophysics and materials
  • Rock Mechanics and Modeling
  • Geochemistry and Elemental Analysis
  • Lichen and fungal ecology
  • Arsenic contamination and mitigation
  • Mining and Resource Management

Universidad Complutense de Madrid
2011-2024

Mineral Resources
2024

Commonwealth Scientific and Industrial Research Organisation
2024

Museo Nacional de Ciencias Naturales
2008-2011

Centro de Investigaciones Energéticas, Medioambientales y Tecnológicas
2008-2009

Centro de Biología Molecular Severo Ochoa
2009

Universidad Autónoma de Madrid
2009

Consejo Superior de Investigaciones Científicas
2009

University of St Andrews
2009

University of Sussex
2009

Stable carbon isotope geochemistry provides important information for the recognition of fundamental exchange processes related to movement in lithosphere and permits elaboration models global cycle. Carbon ratios fluid-deposited graphite are powerful tools unravelling ultimate origin (organic matter, mantle, or carbonates) help constrain fluid history mechanisms involved deposition. Graphite precipitation occurrences results from CO2- and/or CH4-bearing aqueous fluids. Fluid flow can be...

10.1016/j.gsf.2011.11.006 article EN cc-by-nc-nd Geoscience Frontiers 2011-12-13

Abstract Magnetite-(apatite) ore deposits are interpreted as being formed by the crystallization of iron-rich ultrabasic melts, dominantly generated interaction silicate melts with oxidized P-F-SO 4 -bearing sedimentary rocks. This hypothesis is supported geologic evidence, experimental studies, numerical modeling, stable and radiogenic isotope geochemistry, mineralogy, melt- mineral-inclusion data. Assimilation crustal rocks during ascent promotes separation from a magma Fe-rich, Si-Al-poor...

10.1007/s00126-023-01203-w article EN cc-by Mineralium Deposita 2023-09-02

A volcaniclastic formation, known as Cangahua, found in the Andes of Ecuador and Colombia is focused on. The deposit composed moderately cemented fine sand silt‐sized particles. pronounced linear correlation shown between strengh, terms both uniaxial compressive Brazil tensile strengths, dry unit weight deposit. strength unusually high for soil, being 18 29% strength. tensile, compressive, triaxial characteristics depend on initial void ratio degree saturation. As saturation declines from 90...

10.1061/(asce)0733-9410(1988)114:10(1126) article EN Journal of Geotechnical Engineering 1988-10-01

10.1016/j.saa.2012.01.056 article EN Spectrochimica Acta Part A Molecular and Biomolecular Spectroscopy 2012-02-01

The presence of high level heavy metals involves a human healthy risk that could induce chronic diseases. This work reports on the metal contamination due to heaps steel-slag accumulated during more than 40 years in allotments and industrial areas southern part Madrid (Spain). Several slag soil samples were collected an area 10 km² characterized by different conventional (XRD XRF) no so common methods (ESEM, thermoluminescence EDS-WDS). analysis reveal of: (i) important amounts Fe (43%), Mg...

10.1590/s0001-37652010000200003 article EN cc-by Anais da Academia Brasileira de Ciências 2010-06-01

This work presents an integral methodological approach to assess the environmental potential hazards posed by metals and metalloids hosted spolic technosols derived from old tailings a mining operation for galena (PbS, with high Ag contents)-sphalerite (ZnS, varied cohort of trace elements contents) in central Spain. We studied total soluble concentrations spatial distribution Pb, Zn, Cd, As, Fe mineralogy these soils, as well ecotoxicological evaluation means bioassays. The indices...

10.3390/min9060346 article EN Minerals 2019-06-05

Abstract This paper examines the effects of shear stress on structural parameters that define ‘crystallinity’ graphite. The results show highly crystalline graphite samples ground for up to 120 min do not undergo detectable changes in three-dimensional arrangement carbon layers but crystallite sizes ( L c and a ) decrease consistently with increasing grinding time. Grinding also involves particle-size diminution lower temperatures beginning combustion exothermic maxima differential thermal...

10.1180/0026461067060358 article EN Mineralogical Magazine 2006-12-01

The significance of syngenetic and epigenetic graphite occurrences from the Variscan high-temperature/low-pressure Aracena Metamorphic Belt is discussed in framework tectono-thermal evolution this southern zone Iberian Massif. Syngenetic associated with both low- to medium-grade metamorphic rocks (La Umbría series, Precambrian age) high-grade, granulite facies (the Fuente del Oro series a Cambrian calc-silicate series). Epigenetic, fluid-deposited correspond overgrowths on existing grains...

10.1017/s0016756804009896 article EN Geological Magazine 2004-11-01

Arthropod eyes are built of repeating units named ommatidia. Each single ommatidium unit contains a cluster photoreceptor cells surrounded by support and pigment cells. The insect Copium eye ommatidia include additional calcium-phosphate deposits, not described in insects to date, which can be examined today using combined set modern microscopy spectroscopy techniques. Teucrium gnaphalodes L'Her plants, growing central Spain, develop galls induced insects. A survey C. teucrii adult specimens...

10.1100/tsw.2011.9 article EN cc-by The Scientific World JOURNAL 2011-01-01

The geochemical characterization of the mine deposits and soils in metal mining areas is essential order to develop an effective reclamation strategy. determination total potentially toxic element (PTE) content, together with application chemical extraction procedures, can give insight into behavior contaminants after different solutions, as well identify where urgent action needed. This work presents a practical evaluation pollution potential trace elements affected by activities, be used...

10.3390/geosciences11060233 article EN cc-by Geosciences 2021-05-29

The speed at which climate change is happening leading to a demand for new pozzolanic materials that improve the quality of cements and, same time, limit emission greenhouse gases into atmosphere. main objective this work detailed characterization an ignimbrite sample (IGNS) demonstrate its effectiveness as natural pozzolan. To meet objective, series tests were carried out. In first stage, mineral and chemical analyses performed, such petrographic analysis by thin section (TSP), X-ray...

10.3390/ma16041546 article EN Materials 2023-02-13

The phase transition of metavariscite into berlinite has been studied by means different techniques, namely electron probe micro analysis, environmental scanning microscopy, high-temperature X-ray diffraction, differential thermal thermogravimetry, thermoluminescence, and thermo Raman. application these techniques indicates that: (i) from room temperature to 150°C (monoclinic dimorph AlPO4 ⋅ 2H2O) appears as the main phase, (ii) in range 100–300°C starts lose water molecules giving rise form...

10.1080/01411594.2010.490904 article EN Phase Transitions 2010-06-01

Abstract This paper describes a vein-shaped graphite occurrence in which, for the first time, geological, mineralogical and isotopic evidence support its formation by physical remobilization of previously formed syngenetic graphite. The deposit studied is located Spanish Central System it occurs along contact between hydrothermal Ag-bearing quartz vein graphite-bearing quartzite layer. characteristics this differ from those fluid-deposited vein-type mineralization that: (1) flakes are...

10.1180/0026461056940266 article EN Mineralogical Magazine 2005-08-01

The Miocene to Present Mazarrón basin provides a window on the metallogenic role of an evolving magmatic series. High-K calc–alkaline magmas gave rise important cluster Pb–Zn–Ag–Cu vein and stockwork deposits emplaced in dacitic rhyodacitic domes, part complex volcanic–metallogenic province (Au, Hg, Pb–Zn–Cu–Ag, Sn) stretching for ∼150 km along Mediterranean coast SE Spain. By Pliocene time former series had been replaced by intraplate alkaline basaltic volcanism, thus becoming southern...

10.1080/00206814.2013.810379 article EN International Geology Review 2013-06-21

This study aims to use geochemical, mineralogical, ecotoxicological and biological indicators for a comprehensive assessment of the ecological risks related mobility, ecotoxicity bioavailability potentially harmful elements in Lousal mining district. Particularly, toxicity was evaluated using four assays: algae, cytotoxicity assays with HaCaT cell line (dermal), earthworms Daphnia magna. The geochemical mineralogical characterization studied area shows that mine wastes underwent intense...

10.3390/toxics10070353 article EN cc-by Toxics 2022-06-28
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