Cálculo de la anomalía gravimétrica de una cuenca sedimentaria. Su aplicación en la cuenca de Almazán

Almazan Tertiary Basin has a well known geometry based on seismic surveys. From these data, the gravity anomaly due to tertiary sediments has been carried out using the Bhaskara Rao, Prakash, and Ramesh Babu (1990) method. This effect has been removed from the observed gravity map obtaining a new gr...

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Bibliographic Details
Authors: Rey Moral, Carmen, Gómez Ortiz, David, Tejero López, Rosa
Format: article
Publication Date:1998
Country:España
Institution:Universidad de Huelva (UHU)
Repository:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Language:Spanish
OAI Identifier:oai:ariasmontano.uhu.es:10272/10156
Online Access:http://hdl.handle.net/10272/10156
Access Level:Open access
Keyword:Almazan Basin
Gravity anomaly map
Theoretical gravity map
3-D Model
Description
Summary:Almazan Tertiary Basin has a well known geometry based on seismic surveys. From these data, the gravity anomaly due to tertiary sediments has been carried out using the Bhaskara Rao, Prakash, and Ramesh Babu (1990) method. This effect has been removed from the observed gravity map obtaining a new gravity map corresponding to deeper or regional structures (Moho, basement features etc..,). This method provides an useful tool to enhance deep structures which effect would be hidden by overlying sediments