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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Gravity inversion of deep-crust and mantle interfaces in the Three Gorges area
Geodesy and Geodynamics, 2012 To better understand the heterogeneity of deep-crust and mantle interfaces in the region of the Three Gorges, China, we used the Parker-Oldenburg iterative inversion method to invert existing Bouguer gravity data from the Three Gorges area (1 : 500000 ...
Wang Jian +4 more
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Content comparison of patient-reported outcome instruments used to measure burnout [PDF]
, 2015 The aim of this article is to compare the content of patient-reported outcome (PRO) burnout measures and to examine the degree of overlap between them and psychosocial difficulties (PSD) experienced by persons with burnout.
Cieza, A. +2 more
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Depression in Chinese patients with type 2 diabetes: associations with hyperglycemia, hypoglycemia, and poor treatment adherence. [PDF]
, 2015 BackgroundWe hypothesize that depression in type 2 diabetes might be associated with poor glycemic control, in part due to suboptimal self-care. We tested this hypothesis by examining the associations of depression with clinical and laboratory findings ...
Chan, Juliana Cn +15 more
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Effective elastic thickness in the Central Andes. Correlation to orogenic deformation styles and lower crust high-gravity anomaly [PDF]
, 2018 Global studies have assessed the importance of elastic thickness (Te) on orogenic evolution, showing that the style and nature of upper crustal shortening are influenced by the inherited lithospheric strength. Thus, pioneer works have identified that the
Garcia, Hector Pedro Antonio +6 more
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Moho Depth Derived from Gravity Data in the Taiwan Strait Area
Terrestrial, Atmospheric and Oceanic Sciences, 2010 We have constructed are gional Bouguer gravity anomaly map using marine and land data from Tai wan and the Chinese province of Fuchien, as well as SEASAT altimetry-de rived gravity data for the Tai wan Strait and its surrounding area.
Hsien-Hsiang Hsieh +2 more
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