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Inversion of Moho topography in Taiwan using improved Parker-Oldenburg method
Frontiers in Earth ScienceTaiwan is located at the junction between the Philippine Sea Plate and the Eurasian Plate, with intense tectonic movements in the region. A more accurate Moho topography model is significant for the study of the intrinsic genesis within Taiwan’s orogenic
Hangtao Yu +6 more
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Moho Depth Estimation Beneath Tibet From Satellite Gravity Data Based on a Condensation Approach
Earth and Space Science, 2021 We develop an algorithm for a Moho depth recovery from gravity and gravity gradiometry data and apply this method to estimate the Moho depth beneath the Tibetan Plateau.
Wenjin Chen +4 more
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Frontiers in Earth Science, 2023 This study investigates the variations of surface Moho inverted from Bouguer gravity data beneath the northwestern Arabian plate. The results were obtained by applying the 3DINVER program developed in a MATLAB environment using the Parker–Oldenburg ...
Fayez Harash +7 more
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Earth and Space Science, 2023 The Moho is the interface between crust and mantle, and accurate location of the Moho is important for both resource exploration and deep earth condition and structural change investigations. The theory of the traditional Parker‐Oldenburg (P‐O) method is
Weibo Rao +8 more
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Lithosphere, 2022 EIGEN 6C4 gravity anomalies are interpreted to determine the lateral and vertical variations in the crust and upper mantle structure and their influence on the isostasy of the coastal plain, transition zone between the Congo Craton (CC), the Pan-African ...
Willy Lemotio +5 more
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Reformulation of Parker–Oldenburg's method for Earth's spherical approximation
Geophysical Journal International, 2020 SUMMARY Parker–Oldenburg's method is perhaps the most commonly used technique to estimate the depth of density interface from gravity data. To account for large density variations reported, for instance, at the Moho interface, between the ocean seawater density and marine sediments, or between sediments and the underlying bedrock, some ...
Robert Tenzer, Wenjin Chen
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Moho depth inversion in the Tibetan Plateau from high-precision gravity data
Earth and Planetary Physics, 2023 The Tibetan Plateau (TP) is the youngest orogenic belt resulting from a continental collision on the Earth. It is a natural laboratory for studying continental dynamics, such as continental convergence, plate subduction, and plateau uplift. Investigating
HuiYou He +5 more
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Inversion of satellite gravimetric data from Recôncavo-Tucano-Jatobá Basin System
Brazilian Journal of Geology, 2020 Density differences among subsurface rocks cause variations in the gravitational field of Earth, which is known as gravity anomaly. Interpretation of these gravity anomalies allows assessment of the probable depth and shape of the causative body.
Thaíza Pereira Bessoni +2 more
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Age, Depth, and Residual Depth Anomalies in the North Pacific: Implications for Thermal Models of the Lithosphere and Upper Mantle [PDF]
, 1986 We present an empirical basement depth versus age relation for the North Pacific Ocean, based on the statistical treatment of an ocean-wide gridded data set.
Renkin, Miriam K., Sclater, John G.
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Uncertainties and shortcomings of ground surface temperature histories derived from inversion of temperature logs [PDF]
, 2005 Analysing borehole temperature data in terms of ground surface history can add useful information to reconstructions of past climates. Therefore, a rigorous assessment of uncertainties and error sources is a necessary prerequisite for the meaningful ...
Hartmann, Andreas, Rath, Volker
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