Reconciling tectonic shortening, sedimentation and spatial patterns of erosion from 10Be paleo-erosion rates in the Argentine Precordillera

P Val, GD Hoke, JC Fosdick, H Wittmann - Earth and Planetary Science …, 2016 - Elsevier
The temporal evolution of erosion over million-year timescales is key to understand the
development of mountain ranges and adjacent fold-and-thrust belts. While models of …

Reconciling tectonic shortening, sedimentation and spatial patterns of erosion from 10Be paleo-erosion rates in the Argentine Precordillera

P Val, GD Hoke, JC Fosdick, H Wittmann - Earth and Planetary Science …, 2016 - infona.pl
The temporal evolution of erosion over million-year timescales is key to understand the
development of mountain ranges and adjacent fold-and-thrust belts. While models of …

Reconciling tectonic shortening, sedimentation and spatial patterns of erosion from 10Be paleo-erosion rates in the Argentine Precordillera

P Val, GD Hoke, JC Fosdick… - Earth and Planetary …, 2016 - experts.syr.edu
The temporal evolution of erosion over million-year timescales is key to understand the
development of mountain ranges and adjacent fold-and-thrust belts. While models of …

Reconciling tectonic shortening, sedimentation and spatial patterns of erosion from 10Be paleo-erosion rates in the Argentine Precordillera

P Val, GD Hoke, JC Fosdick… - Earth and Planetary …, 2016 - ui.adsabs.harvard.edu
The temporal evolution of erosion over million-year timescales is key to understand the
development of mountain ranges and adjacent fold-and-thrust belts. While models of …

Reconciling tectonic shortening, sedimentation and spatial patterns of erosion from 10Be paleo-erosion rates in the Argentine Precordillera

P Val, GD Hoke, JC Fosdick… - Earth and Planetary …, 2016 - gfzpublic.gfz-potsdam.de
The temporal evolution of erosion over million-year timescales is key to understand the
development of mountain ranges and adjacent fold-and-thrust belts. While models of …

[PDF][PDF] USA 13244 6 7 Julie C. Fosdickb 8 bDept. of Geological Sciences, Indiana University, 1001 East 10th Street, Bloomington, 9 IN, USA 47405 10

H Wittmannc, P Val - gfzpublic.gfz-potsdam.de
The temporal evolution of erosion over million-year timescales is key to understand the 26
development of mountain ranges and adjacent fold-and-thrust belts. While models of 27 …