The Isostatic Residual Gravity Anomaly of the Central Andes, 12° to 29° S: A Guide to Interpreting Crustal Structure and Deeper Lithospheric Processes
Author:
Affiliation:
1. a Department of Geology , Florida International University , Miami, Florida, 33199
Publisher
Informa UK Limited
Subject
Geology
Link
https://www.tandfonline.com/doi/pdf/10.1080/00206819909465152
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1. Crustal structure of the high Andes in the North Pampean flat slab segment from magnetic and gravity data;Journal of South American Earth Sciences;2017-01
2. Hinterland basin formation and gravitational instabilities in the central Andes: Constraints from gravity data and geodynamic models;Geodynamics of a Cordilleran Orogenic System: The Central Andes of Argentina and Northern Chile;2015
3. Geophysical characterization of the upper crust in the transitional zone between the Pampean flat slab and the normal subduction segment to the south (32–34°S): Andes of the Frontal Cordillera to the Sierras Pampeanas;Geological Society, London, Special Publications;2014-02-06
4. Finite element modeling of neotectonics in New Zealand;Journal of Geophysical Research: Solid Earth;2002-12
5. Effect of windowing on lithosphere elastic thickness estimates obtained via the coherence method: Results from northern South America;Journal of Geophysical Research: Solid Earth;2002-11
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