In the present paper, we investigate the Airy type isostatic compensation scheme for three interfaces:water-sediments, sediments-crust and crust-mantle, using forward modelling to calculate the isostaticanomaly with different approximations of Parkers expression in the Argentine continentalmargin. The isostatic anomaly is estimated as the residue between the observed free air anomaly andthe calculated free air anomaly through the sum of the contributions from the tree interfaces.After that, we perform the inversion of the isostatic anomaly in order to find the deflection of theMoho necessary to compensate it (or minimize it) using one term of Parkers expression in the inversion,as an experiment to test the numerical methods. The Moho here c...
The Río de la Plata estuarine has been the epicenter of the 30 November 2018 intra-crustal earthquak...
The global gravity and crustal models are used in this study to determine the regional Moho model. F...
We developed a 3D density model of the continental crust, the subducted plate and the upper mantle o...
In this work we present a new, alternative methodology for performing isostatic studies by means of ...
Mapping an arbitrary interface separating two homogeneous media, traditionally uses the downward con...
Isostatic gravity anomalies provide a measure of the Earth's gravity field free from the gravitation...
Gravimetric methods applied for Moho recovery in areas with sparse and irregular distribution of sei...
Four theoretical models isostatically compensated were prepared and compared between themselves in o...
The Mohorovicic discontinuity (Moho) is the surface that limits the Earth’s crust and mantle. It is ...
The Salado Basin, placed in Buenos Aires province, Argentina, is one of the most studied sedimentary...
Abstract.- Four theoretical models isostatically compensated were prepared and compared between them...
Salado Basin, placed in Buenos Aires province, Argentina, is one of the most studiedsedimentary basi...
The Process-Oriented Gravity Modelling (POGM) technique represents a useful way to distinguish the c...
This paper presents the estimates of effective elastic thickness (T e) from free-air anomalies/geoid...
In this paper, we analyze an E-W gravity section at 39° South latitude. It extends from the western ...
The Río de la Plata estuarine has been the epicenter of the 30 November 2018 intra-crustal earthquak...
The global gravity and crustal models are used in this study to determine the regional Moho model. F...
We developed a 3D density model of the continental crust, the subducted plate and the upper mantle o...
In this work we present a new, alternative methodology for performing isostatic studies by means of ...
Mapping an arbitrary interface separating two homogeneous media, traditionally uses the downward con...
Isostatic gravity anomalies provide a measure of the Earth's gravity field free from the gravitation...
Gravimetric methods applied for Moho recovery in areas with sparse and irregular distribution of sei...
Four theoretical models isostatically compensated were prepared and compared between themselves in o...
The Mohorovicic discontinuity (Moho) is the surface that limits the Earth’s crust and mantle. It is ...
The Salado Basin, placed in Buenos Aires province, Argentina, is one of the most studied sedimentary...
Abstract.- Four theoretical models isostatically compensated were prepared and compared between them...
Salado Basin, placed in Buenos Aires province, Argentina, is one of the most studiedsedimentary basi...
The Process-Oriented Gravity Modelling (POGM) technique represents a useful way to distinguish the c...
This paper presents the estimates of effective elastic thickness (T e) from free-air anomalies/geoid...
In this paper, we analyze an E-W gravity section at 39° South latitude. It extends from the western ...
The Río de la Plata estuarine has been the epicenter of the 30 November 2018 intra-crustal earthquak...
The global gravity and crustal models are used in this study to determine the regional Moho model. F...
We developed a 3D density model of the continental crust, the subducted plate and the upper mantle o...