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

dc.contributor.authorRey Moral, Carmen
dc.contributor.authorGómez Ortiz, David
dc.contributor.authorTejero López, Rosa
dc.date.accessioned2015-03-25T12:51:09Z
dc.date.available2015-03-25T12:51:09Z
dc.date.issued1998
dc.description.abstractAlmazan 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 sedimentsen_US
dc.identifier.urihttp://hdl.handle.net/10272/10156
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherAlmazan Basinen_US
dc.subject.otherGravity anomaly mapen_US
dc.subject.otherTheoretical gravity mapen_US
dc.subject.other3-D Modelen_US
dc.titleCálculo de la anomalía gravimétrica de una cuenca sedimentaria. Su aplicación en la cuenca de Almazánen_US
dc.titleThe computation of sedimentary basin gravity anomaly. Its aplication to the almazan basineng
dc.typejournal articleen_US
dspace.entity.typePublication

Files

Original bundle

Now showing 1 - 1 of 1
Loading...
Thumbnail Image
Name:
Calculo.pdf
Size:
1.05 MB
Format:
Adobe Portable Document Format