Abstract
The Northern Andean Block is the result of complex tectonic interaction between the Farallon-Nazca, South American, and Caribbean Plates. Abundant late Cenozoic volcanism (and associated hypabyssal porphyritic plutonism), beginning in the mid- to late Miocene, is the result of subduction-related mantle-derived magmatic activity, superimposed upon a compositionally varied and structurally complex basement during the late stages of the Northern Andean orogeny. Tectonic consolidation and subduction of the segmented Nazca Plate during the late Miocene-Pliocene led to conformation of the modern-day Colombian segment of the Northern Andean Volcanic Zone. The Colombian arc segment represents the northernmost expression of subduction-related volcanism within South America’s Andean Cordillera.
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Abbreviations
- ACPB:
-
Amagá-Cauca-Patía
- AFC:
-
Assimilations by fractional crystallization
- AFM:
-
Diagram alkali-iron-magnesium
- AFS:
-
Algeciras fault system
- AOC:
-
Altered oceanic crust
- AVZ:
-
Austral Volcanic Zone
- BAU:
-
Baudó terrane
- Ca:
-
(circa) Approximately
- CAM:
-
Caribbean mountain terrane
- CA-VA:
-
Cajamarca-Valdivia terrane
- CC:
-
Central Cordillera
- CET:
-
Colombia-Ecuador trench
- CG:
-
Cañasgordas terrane
- CS:
-
Carbonate-rich sediments
- CV:
-
Cauca Valley
- CVZ:
-
Central Volcanic Zone
- DA:
-
Dagua terrane
- E:
-
East
- E.g.:
-
For example (exempli gratia)
- EC:
-
Eastern Cordillera
- ENE:
-
East northeast
- Et al:
-
And others (et alia)
- Fig:
-
Figure
- Fm.:
-
Formation
- GA:
-
Macizo de Garzón
- GOR:
-
Gorgona terrane
- GPa:
-
GigaPascal
- GU-FA:
-
Guajira-Falcón terranes
- HFS:
-
High-field strength
- HFSE:
-
High-field-strength elements
- HIMU:
-
High U/Pb mantle
- HREE:
-
Heavy rare earth elements
- HS:
-
Hemipelagic sediments
- I.E:
-
In essence (id est)
- K:
-
Cretaceous
- Km:
-
Kilometers
- LCC:
-
Lower continental crust
- LIL:
-
Large-ion lithophile
- LILE:
-
Large-ion lithophile elements
- LREE:
-
Light rare earth elements
- Ma:
-
Mega-annum
- MMB:
-
Middle Magdalena Basin
- MORB:
-
Mid-ocean-ridge basalt
- MSP:
-
Maracaibo subplate
- N:
-
Neogene
- NAB:
-
Northern Andean Block
- NE:
-
Northeast
- NNE:
-
North northeast
- NVZ:
-
Northern Volcanic Zone
- NW:
-
Northwest
- OIB:
-
Ocean island basalt
- P:
-
Paleogene
- P:
-
Pressure
- PA:
-
Panamá terrane
- Pa:
-
Pascal
- PCB:
-
Panamá-Chocó Block
- Pz:
-
Paleozoic
- RA:
-
Rear arc
- REE:
-
Rare earth element
- RO:
-
Romeral terrane
- SE:
-
Southeast
- SJ:
-
San Jacinto terrane
- SL:
-
San Lucas Block
- SM:
-
Sierra Nevada de Santa Marta
- SN:
-
Sinú terrane
- SS:
-
Subducted sediments
- SVZ:
-
South Volcanic Zone
- SW:
-
Southwest
- T:
-
Temperature
- TAS:
-
Total alkali-silica
- UCC:
-
Upper continental crust
- VF:
-
Volcanic front
- W:
-
West
- WBZ:
-
Wadati-Benioff zone
- WC:
-
Western Cordillera
- WSW:
-
West southwest
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Marín-Cerón, M.I., Leal-Mejía, H., Bernet, M., Mesa-García, J. (2019). Late Cenozoic to Modern-Day Volcanism in the Northern Andes: A Geochronological, Petrographical, and Geochemical Review. In: Cediel, F., Shaw, R.P. (eds) Geology and Tectonics of Northwestern South America. Frontiers in Earth Sciences. Springer, Cham. https://doi.org/10.1007/978-3-319-76132-9_8
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