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Uplifted Pleistocene Marine Terraces at Active Margins: Modeling Reveals the Effects of Sea Reoccupation and Coseismic Uplift on Uplift Rate Calculation

Abstract Uplifted Pleistocene marine terrace sequences are used to quantify uplift rates along active margins by knowing terrace age and elevation, and sea level (SL) position at the time of terrace formation. When terraces are undated, ages are assigned by correlating terraces at progressively high...

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I tiakina i:
Ngā taipitopito rārangi puna kōrero
Ngā kaituhi matua: Silvia Crosetto, Albert deMontserrat, Onno Oncken
Hōputu: Artigo
Reo:Inglês
I whakaputaina: Wiley 2024-04-01
Rangatū:Geochemistry, Geophysics, Geosystems
Ngā marau:
Urunga tuihono:https://doi.org/10.1029/2023GC011036
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