English
 
Privacy Policy Disclaimer
  Advanced SearchBrowse

Item

ITEM ACTIONSEXPORT
  North Patagonian Massif, Argentina : Lithospheric 3D gravity modelling using upper-mantle density constraints

Gomez Dacal, M. L., Tocho, C., Aragón, E., Bott [Sippel], J., Scheck-Wenderoth, M. (2020): North Patagonian Massif, Argentina: Lithospheric 3D gravity modelling using upper-mantle density constraints.
https://doi.org/10.5880/GFZ.4.5.2020.002

Item is

Files

show Files

Locators

show
hide
Locator:
https://www.doi.org/10.1016/j.tecto.2017.02.011 (Supplementary material)
Description:
Supplement to Gomez Dacal, M. L. et al. (2017)

Creators

show
hide
 Creators:
Gomez Dacal, Maria Laura1, Author              
Tocho, Claudia2, Author
Aragón, Eugenio2, Author
Bott [Sippel], Judith1, Author              
Scheck-Wenderoth, Magdalena1, Author              
Affiliations:
14.5 Basin Modelling, 4.0 Geosystems, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_146042              
2External Organizations, ou_persistent22              

Content

show
hide
Free keywords: 3D gravity modelling, Crustal configuration, North Patagonian Massif, compound material > rock > composite genesis rock > metamorphic rock, compound material > rock > igneous rock, compound material > rock > sedimentary rock, science > natural science > earth science > geology, science > natural science > earth science > geophysics
 Abstract: We present a 3-D lithospheric-scale data-constrained structural model covering the area of North Patagonian Massif Plateau (NPM) and its surroundings. These data are supplementary material to “Lithospheric 3D gravity modelling using upper-mantle density constraints: Towards a characterization of the crustal configuration in the North Patagonian Massif area, Argentina” (Gómez Dacal et al. 2017). The North Patagonian Massif (NPM), in central Argentina, includes a plateau of an average altitude of 1200 m.a.s.l. mostly surrounded by basins that stand between 500 to 700 m below it. Geological observations and previous works indicate that the present-day elevation of the plateau was reached in the Paleogene by a sudden uplift that did not involve noticeable deformation. To gain insight into the causes of the uplift and the geodynamic development of the area, it is necessary to characterize the present-day configuration of the lithosphere.

Details

show
hide
Language(s): eng - English
 Dates: 2020
 Publication Status: Finally published
 Pages: -
 Publishing info: Potsdam : GFZ Data Services
 Table of Contents: -
 Rev. Type: -
 Identifiers: DOI: 10.5880/GFZ.4.5.2020.002
 Degree: -

Event

show

Legal Case

show

Project information

show

Source

show