The isostatic residual gravity anomaly of the central Andes, 12 degrees to 29 degrees S: A guide to interpreting crustal structure and deeper lithospheric processes Article

Whitman, D. (1999). The isostatic residual gravity anomaly of the central Andes, 12 degrees to 29 degrees S: A guide to interpreting crustal structure and deeper lithospheric processes . INTERNATIONAL GEOLOGY REVIEW, 41(5), 457-475. 10.1080/00206819909465152

keywords

  • BENEATH
  • BOLIVIA
  • FLEXURAL RIGIDITY
  • GEOMETRY
  • Geology
  • MODEL
  • NORTHWEST-ARGENTINA
  • PERUVIAN ANDES
  • Physical Sciences
  • SUBDUCTED NAZCA PLATE
  • Science & Technology
  • TECTONICS
  • THICKNESS

Digital Object Identifier (DOI)

publisher

  • TAYLOR & FRANCIS INC

start page

  • 457

end page

  • 475

volume

  • 41

issue

  • 5