LITHO1. 0: An updated crust and lithospheric model of the Earth
ME Pasyanos, TG Masters, G Laske… - Journal of Geophysical …, 2014 - Wiley Online Library
We present the LITHO1. 0 model, which is a 1° tessellated model of the crust and uppermost
mantle of the Earth, extending into the upper mantle to include the lithospheric lid and …
mantle of the Earth, extending into the upper mantle to include the lithospheric lid and …
An integrated approach to unravel the structural controls on groundwater potentialities in hyper-arid regions using satellite and land-based geophysics: a case study in …
Groundwater exploration is the most promising way to overcome water scarcity in hyper-arid
regions around the world. Due to the scarcity of hydrogeological information in these …
regions around the world. Due to the scarcity of hydrogeological information in these …
Heat flux distribution of Antarctica unveiled
Antarctica is the largest reservoir of ice on Earth. Understanding its ice sheet dynamics is
crucial to unraveling past global climate change and making robust climatic and sea level …
crucial to unraveling past global climate change and making robust climatic and sea level …
The breakup of East Gondwana: Assimilating constraints from Cretaceous ocean basins around India into a best‐fit tectonic model
AD Gibbons, JM Whittaker… - Journal of geophysical …, 2013 - Wiley Online Library
Published models for the Cretaceous seafloor‐spreading history of East Gondwana result in
unlikely tectonic scenarios for at least one of the plate boundaries involved and/or violate …
unlikely tectonic scenarios for at least one of the plate boundaries involved and/or violate …
Combined gravimetric–seismic crustal model for Antarctica
The latest seismic data and improved information about the subglacial bedrock relief are
used in this study to estimate the sediment and crustal thickness under the Antarctic …
used in this study to estimate the sediment and crustal thickness under the Antarctic …
S‐velocity model and inferred Moho topography beneath the Antarctic Plate from Rayleigh waves
M An, DA Wiens, Y Zhao, M Feng… - Journal of …, 2015 - Wiley Online Library
Abstract Since 2007/2008, seismographs were deployed in many new locations across
much of Antarctica. Using the records from 122 broadband seismic stations, over 10,000 …
much of Antarctica. Using the records from 122 broadband seismic stations, over 10,000 …
Aquifer recharge, depletion, and connectivity: Inferences from GRACE, land surface models, and geochemical and geophysical data
Abstract Data from the Gravity Recovery and Climate Experiment (GRACE) and outputs of
the CLM4. 5 model were used to estimate recharge and depletion rates for large aquifers …
the CLM4. 5 model were used to estimate recharge and depletion rates for large aquifers …
The crust and upper mantle structure of central and West Antarctica from Bayesian inversion of Rayleigh wave and receiver functions
We construct a new seismic model for central and West Antarctica by jointly inverting
Rayleigh wave phase and group velocities along with P wave receiver functions. Ambient …
Rayleigh wave phase and group velocities along with P wave receiver functions. Ambient …
New Antarctic gravity anomaly grid for enhanced geodetic and geophysical studies in Antarctica
M Scheinert, F Ferraccioli, J Schwabe… - Geophysical …, 2016 - Wiley Online Library
Gravity surveying is challenging in Antarctica because of its hostile environment and
inaccessibility. Nevertheless, many ground‐based, airborne, and shipborne gravity …
inaccessibility. Nevertheless, many ground‐based, airborne, and shipborne gravity …
The crustal thickness of West Antarctica
P‐to‐S receiver functions (PRFs) from the Polar Earth Observing Network (POLENET) GPS
and seismic leg of POLENET spanning West Antarctica and the Transantarctic Mountains …
and seismic leg of POLENET spanning West Antarctica and the Transantarctic Mountains …