Geodynamics Modeling
The Earth's mantle is the thickest yet the most enigmatic layer of our planet. Mantle xenoliths and some parts of ophiolites surely are great help, but what about the unfolded huge remainder?
We can only rely on two methods to tackle such a complexity and shed a light on the mantle dynamics. One is deep seismology, the other is geodynamics modeling. Find out through my conference posters what geodynamics modeling can achieve.
AGU Fall Meeting 2022
Recycled basaltic material in mantle plumes explains the appearance of the X-discontinuity inthe upper mantle beneath the Hawaiian hotspot: 2D geodynamic numerical models
New findings on the potential for recycled material to be entrained in the mid-upper mantle beneath the Hawaiian hotspot.
Ada Lovelace Workshop 2022
Recycled basaltic material in mantle plumes explains the appearance of the X-discontinuity in the upper mantle: 2D geodynamic numerical models
The investigation on the potential for recycled material entrainment in the mid-upper mantle is complemented by new, whole-plume models.
AGU Fall Meeting 2021
The segregation of recycled basaltic material within mantle plumes explains the detection of the X-Discontinuity beneath hotspots: 2D geodynamic simulations
AGU 2021 Spotlight Interview
Ever wondered what's to know about the Hawaiian mantle plume and the X-Discontinuity in two minutes? Meet me highlighting the main takeaways of my poster and find out!
Exploration Geology MSc Thesis, 2020
The Andean Subduction Zone
Find out my modeling results from my Master's Degree Research Intern. Don't forget to watch the presentation in animation mode.