Daniele Giordano

ORCID: 0000-0003-1271-5516
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About
Contact & Profiles
Research Areas
  • Geological and Geochemical Analysis
  • Glass properties and applications
  • High-pressure geophysics and materials
  • earthquake and tectonic studies
  • Material Dynamics and Properties
  • Mineralogy and Gemology Studies
  • Geological formations and processes
  • Cultural Heritage Materials Analysis
  • Building materials and conservation
  • Geology and Paleoclimatology Research
  • Geochemistry and Geologic Mapping
  • Hydrocarbon exploration and reservoir analysis
  • Pancreatic and Hepatic Oncology Research
  • Cancer Immunotherapy and Biomarkers
  • Immunotherapy and Immune Responses
  • Landslides and related hazards
  • Cancer Research and Treatments
  • Geological Modeling and Analysis
  • CO2 Sequestration and Geologic Interactions
  • Methane Hydrates and Related Phenomena
  • Geological Formations and Processes Exploration
  • Geological and Geophysical Studies Worldwide
  • Geomagnetism and Paleomagnetism Studies
  • Rheology and Fluid Dynamics Studies
  • Geotechnical and Geomechanical Engineering

University of Campania "Luigi Vanvitelli"
2014-2025

Institute of Geosciences and Earth Resources
2016-2024

University of Turin
2015-2024

National Research Council
2016-2024

Azienda Ospedaliera Citta' della Salute e della Scienza di Torino
2015-2022

Institute of Science and Technology for Ceramics
2022

Universidade de São Paulo
2020-2021

Istituto Nazionale di Geofisica e Vulcanologia
2004-2019

University of Naples Federico II
2008-2019

Geociencias Barcelona
2010-2014

10.1016/j.epsl.2008.03.038 article EN Earth and Planetary Science Letters 2008-04-11

10.1016/s0012-821x(03)00042-6 article EN Earth and Planetary Science Letters 2003-03-30

Storage and transport of silicate melts in the Earth's crust their emplacement on planet's surface occur almost exclusively at sub-liquidus temperatures. At these conditions, undergo crystallization under a wide range cooling-rates, deformation-rates, oxygen fugacities (fO2). Oxygen fugacity is known to influence thermodynamics kinetics magmas lavas. Yet, its rheology remains largely uncharted. We present first rheological characterization crystallizing lavas along natural cooling paths...

10.1016/j.epsl.2018.01.023 article EN cc-by-nc-nd Earth and Planetary Science Letters 2018-02-06

The majority of basaltic magmas stall in the Earth's crust as a result rheological evolution caused by crystallization during transport. However, relationships between crystallinity, rheology and eruptibility remain uncertain because it is difficult to observe dynamic magma real time. Here, we present in-situ 4D data for crystal growth kinetics textural pyroxene trachybasaltic high-temperature experiments under water-saturated conditions at crustal pressures. We dendritic on initially...

10.1038/s41467-022-30890-8 article EN cc-by Nature Communications 2022-06-10

Abstract The 2021 Tajogaite eruption of Cumbre Vieja (La Palma, Spain) was typified by the emission low viscosity lavas that flowed at high velocities and inundated a large area. We experimentally investigated rheological evolution melt feeding through concentric cylinder viscometry to understand exceptional flowing ability these constrain its emplacement dynamics. conducted set cooling deformation experiments different rates (from 0.1 10 °C/min), isothermal subliquidus dwell temperatures...

10.1029/2022gl100970 article EN cc-by-nc-nd Geophysical Research Letters 2023-02-14

The prediction of viscosity in silicate melts, over the range conditions found nature, remains one most challenging and elusive goals Earth Sciences. We present a strategy for fitting non-Arrhenian models [e.g., Vogel-Tammann-Fulcher (VTF) or Adam-Gibbs (AG)] to data that can be employed toward full multicomponent model melt viscosity. Our postulate is high-T viscosities melts converge common value. implications are twofold. First, number composition-dependent parameters reduced by third....

10.2138/am-2003-8-924 article EN American Mineralogist 2003-08-01

10.1016/j.epsl.2004.07.017 article EN Earth and Planetary Science Letters 2004-09-01

Transport properties of natural silicate melts at super-liquidus temperatures are reasonably well understood. However, migration and transport in the Earth’s crust its surface generally occur sub-liquidus settings where undergo crystallization under various cooling and/or decompression conditions. In such dynamic situations occurrence processes as release latent heat during phase changes, viscous heating, thermal advection -inertia, changing capacity, all represent potential influences on...

10.1016/j.gca.2016.09.022 article EN cc-by-nc-nd Geochimica et Cosmochimica Acta 2016-09-24

A hallmark of cancer, including pancreatic ductal adenocarcinoma (PDA), is a massive stromal and inflammatory reaction. Many efforts have been made to identify the anti- or protumoral role cytokines immune subpopulations within stroma. Here, we investigated interleukin-17A (IL17A) its effect on tumor fibroblasts microenvironment. We used spontaneous PDA mouse model (KPC) crossed IL17A knockout mice show an extensive desmoplastic reaction, without impaired infiltration. Macrophages,...

10.1073/pnas.2020395118 article EN Proceedings of the National Academy of Sciences 2021-02-01
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