Moho depth and equivalent elastic thickness of the lithosphere over the Vema Channel: A new evidence of an aborted ridge

Author:

Constantino Renata Regina,Costa Iago Sousa LimaORCID,Hackspacher Peter Christian,de Souza Iata Anderson

Funder

CAPES

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference39 articles.

1. ETOPO1 1 Arc-minute Global Relief Model: Procedures, Data Sources and Analysis;Amante,2009

2. Brazilian and African passive margins of the Central Segment of the South Atlantic Ocean: kinematic constraints;Aslanian;Tectonophysics,2009

3. Tectonic evolution and subsidence history of the rio-grande rise;Barker;Initial Rep. Deep Sea Drill. Proj.,1983

4. The oceanic segment of the Southern Brazilian margin: morpho-structural domains and their tectonic significance;Bassetto;Atl. Rifts Continent. Margin.,2000

5. Spectral and classical methods in the evaluation of Moho undulations from gravity data: the NE Italian Alps and isostasy;Braitenberg;J. Geodyn.,1997

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