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Structure of the continental margin of southwestern Panama
David A. Okaya
*
,
Zvi Ben-Avraham
*
Corresponding author for this work
School of the Environment and Earth Sciences
Stanford University
Lawrence Berkeley National Laboratory
Research output
:
Contribution to journal
›
Article
›
peer-review
11
Scopus citations
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Keyphrases
Acoustic Basement
60%
Caribbean
20%
Chiriqui
60%
CoCos
20%
Cocos Plate
40%
Coiba Island
40%
Continental Margin
100%
Continental Shelf
80%
Costa Rica
20%
Erosional Surface
20%
Farallon Plate
40%
High-angle Normal Faults
20%
Left Lateral Sectionectomy
20%
Mid-Miocene
20%
Mid-Tertiary
40%
Multichannel Seismic Profiles
20%
Nazca
20%
Normal Faulting
20%
Ocean Floor
20%
Outer Continental Shelf
20%
Panama
100%
Plate Motions
20%
Reflector
20%
Sedimentary Basin
20%
Sedimentary Sequence
20%
Seismic Profiles
40%
Shelf Break
20%
Shelf Deposit
20%
Subduction
60%
Transform Plate Boundary
40%
Triple Junction
40%
Volcanic Basement
40%
Earth and Planetary Sciences
Cocos Plate
28%
Continental Shelf
100%
Costa Rica
14%
Miocene
14%
Panama
100%
Plate Boundary
14%
Plate Motion
14%
Sea Bed
14%
Sedimentary Basin
14%
Sedimentary Sequence
14%
Shelf Break
14%
Tertiary Period
14%
Triple Junction
28%