Seismic constraints on the thermal structure of the Italian crust
- Author(s)
- C. Gao, G. Diaferia, F. Cammarano, N. Piana Agostinetti, V. Lekic, I. Molinari
- Abstract
Temperature distribution at depth is of key importance to characterize
the crust, defining its role and behavior in relation to neighboring
plates and the mantle underneath. Temperature can be retrieved by heat
flow measurements in boreholes, but data are sparse and shallow and do
not provide the necessary coverage and reliability, especially in active
and geologically recent areas. Laboratory data and thermodynamic
modeling demonstrate that temperature exerts a strong control on the
seismic properties of rocks, supporting the hypothesis that seismic data
can be used to unravel the thermal structure of the crust. We use
Rayleigh wave dispersion curves (SWD) and receiver functions (RFs),
jointly inverted with a trans-dimensional Monte Carlo Markov Chain
algorithm, to retrieve the VS and VP/VS
at crustal depth for the Italian peninsula. Except for the areas where
the geological complexities have hampered the retrieval of a
satisfactory model, the obtained subsurface models are exploited for the
crustal characterization. The high values (>1.9) of
VP/VS suggest a relevant role of filled-fluid
cracks in the middle and lower crust. Intra-crustal discontinuities
associated with large values of VP/VS are
interpreted as the α-β quartz transition and used for the
estimation of geothermal gradients. The use of thermodynamics to
translate shear-wave velocities into temperature leads to similar
estimates, in agreement with the known tectonic and geodynamic setting
of the Italian Peninsula. Seismological data are therefore a viable
alternative to heat flow measurements for the thermal characterization
of the crust.
- Organisation(s)
- Department of Geology
- External organisation(s)
- University of Maryland, College Park, Università Degli Studi Roma Tre, University of Copenhagen, Dublin Institute for Advanced Studies, Istituto Nazionale di Fisica Nucleare (INFN), Roma
- Publication date
- 12-2018
- Peer reviewed
- Yes
- Austrian Fields of Science 2012
- 105102 General geophysics
- Keywords
- Portal url
- https://ucrisportal.univie.ac.at/en/publications/1c6fb070-cdb9-409f-9f24-6059df0f61bb