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Moho depth and crustal thinning in the Marmara Sea region from gravity data inversion ArchiMer
Kende, Julia; Henry, P.; Bayrakci, G.; Ozeren, M. S.; Grall, C.
The free-air gravity in the Marmara Sea reveals that the low density of sedimentary basins is partly compensated in the lower crust. We compiled geophysical upper crust studies to determine the sediment basin geometries in and around the Marmara Sea and corrected the gravity signal from this upper crust geology with the Parker method. Then, assuming long wavelength anomalies in the residual gravity signal is caused by variations in the Moho topography, we inverted the residual to build the Moho topography. The result shows that the Moho is uplifted on an area greater than the Marmara Sea with a maximum crust thinning beneath the basins where the Moho is at about 25 km, 5 km above the reference depth. We then evaluated the Neogene extension by comparing the...
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Ano: 2017 URL: https://archimer.ifremer.fr/doc/00371/48188/48303.pdf
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MARSITECRUISE R/V Pourquoi pas? October 28th – November 17th, 2014. Leg 3 - Six-Month Cruise Report ArchiMer
Henry, Pierre; Kende, Julia.
Leg 3 was dedicated to core sampling and to the recovery of geophysical instrumentation. The general objective of core analysis will be to ground truth interpretations of high-resolution seismic data and to identify and date sedimentary events related to earthquakes.
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Ano: 2015 URL: https://archimer.ifremer.fr/doc/00434/54534/55904.pdf
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