ISOSTATIC REBOUND DUE TO TECTONIC DENUDATION - A VISCOUS-FLOW MODEL OF A LAYERED LITHOSPHERE Article

WDOWINSKI, S, AXEN, GJ. (1992). ISOSTATIC REBOUND DUE TO TECTONIC DENUDATION - A VISCOUS-FLOW MODEL OF A LAYERED LITHOSPHERE . TECTONICS, 11(2), 303-315. 10.1029/91TC02341

cited authors

  • WDOWINSKI, S; AXEN, GJ

sustainable development goals

authors

publication date

  • April 1, 1992

published in

keywords

  • ANGLE NORMAL FAULTS
  • BASIN
  • CALIFORNIA
  • CONTINENTAL LITHOSPHERE
  • CORE COMPLEX
  • DEFORMATION
  • EASTERN NEVADA
  • EXTENSION
  • Geochemistry & Geophysics
  • MANTLE
  • Physical Sciences
  • RANGE PROVINCE
  • Science & Technology

Digital Object Identifier (DOI)

publisher

  • AMER GEOPHYSICAL UNION

start page

  • 303

end page

  • 315

volume

  • 11

issue

  • 2