CLR person interests, research and publications
Researcher
Research interests
- Geophysical characterization of accretionary and collisional orogenic systems
- Architecture of continental lithosphere with forward and inverse modeling of gravity and magnetic anomalies
- Structural geology and tectonics of orogenic systems
Current research topics
My work is focused on geological interpretation of the Earth's gravity and magnetic fields by studying potential field data combined with structural analysis, magmatic rock geochemistry, petrophysical data and seismics. This multidisciplinary approach constrains the structure of the lithosphere. My research strength is the treatment, the interpretation and the synthesis of large sets of geophysical and geological data in order to model (forward and inverse modeling) the structure of the lithosphere from regional to large scale. The obtained geophysical models contribute to reconstruct consistent tectonic evolution of accretionary and collisional orogenic systems.
Research projects
The Central Asian Orogenic Belt (CAOB) is an accretionary orogen covering one third of Asia. Guy et al. (2014) demonstrate by the correlation between geology and potential field data that the systematic use of lithostratigraphic terranes to define the CAOB is not appropriate.
Selected segments of Euroasian orogenic system are used to constrain relative contribution of contrasting processes of continental construction in collisional and accretionary orogenic systems. Principal objectives of the proposal are: (i) identification of the individual terranes, kinematic analysis of their movements and characterization of deformation style connected with their amalgamation; (ii) estimation of net crustal growth vs. recycling of preexistent crustal material.
On the modern Earth, continental crust is created mainly at subduction zones. Here, release of aqueous fluid from dehydrating oceanic crust causes melting in the mantle wedge and generates the calc-alkaline magmas that evolve into granitoid continental crust. This project aims to understand crustal growth and possible crustal construction mechanisms, using the Mongolian and Chinese tract of the Central Asian Orogenic Belt (CAOB) as an example. The main questions raised here are: What were the cause, rate and timing of continental growth in the CAOB?
The project will study timing and dynamics of collisional processes in the Tuareg Shield (central Hoggar, Algeria). The data will be used for evaluation of the models of multiple subductions in the Tuareg Shield and for understanding whether the closure of different oceanic domains in this part of West Gondwana was synchronous or not. The results of the project will provide improved picture of Neoproterozoic geodynamic evolution of northern part of the western Gondwana suture.
This project investigates the lithospheric structure of the Mongolian collage part of the Central Asian Orogenic Belt, shaped by multiple accretion and collision processes. To decode this orogen, we will combine cluster analysis with geophysical inverse and forward modelling to address the occurrence of a felsic relaminant and its extent, and to examine the suture zones and subductions involved in the Mongolian oroclinal bending.