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 Volume 2 Chapter 10

Chapter  10


Cretaceous record from a Mariana​​​ to an Andean–Type Margin in the Central Cordillera of the Colombian Andes   

Agustín CARDONA Santiago LEÓN, Juan S. JARAMILLO, Victor A. VALENCIA, Sebastian ZAPATA, Andrés PARDO–TRUJILLO, Axel K. SCHMITT, Dany MEJÍA, and Juan Camilo ARENAS

https://doi.org/10.32685/pub.esp.36.2019.10


ISBN impreso obra completa: 978-958-52959-1-9

ISBN digital obra completa: 978-958-52959-6-4

ISBN impreso Vol. 2: 978-958-52959-3-3

ISBN digital Vol. 2: 978-958-52959-8-8​


Citation is suggested as: 

Cardona, A., León, S., Jaramillo, J.S., Valencia, V., Zapata, S., Pardo–Trujillo, A., Schmitt, A.K., Mejía, D. & Arenas, J.C. 2020. Cretaceous record from a Mariana– to an Andean–type margin in the Central Cordillera of the Colombian Andes. In: Gómez, J. & Pinilla–Pachon, A.O. (editors), The Geology of Colombia, Volume 2 Mesozoic. Servicio Geológico Colombiano, Publicaciones Geológicas Especiales 36, p. 335–373. Bogotá. https://doi.org/10.32685/pub.esp.36.2019.10


Download chapter  ​​     ​Download sup​plementary information  ​​​ 

Download EndNote reference​ ​​



Abstract


The Cretaceous tectonic evolution of the western margin of South America involves a shift from an extensional convergent margin toward a more compressional setting that marks the beginning of the Andean Orogeny. In the Colombian Andes, this changing scenario is recorded in the Cretaceous sedimentary and magmatic rocks of the Central Cordillera. A review of field relationships, together with analysis of integrated provenance constraints, including sandstone petrography and detrital zircon geochronology from various localities, suggests that during the Early Cretaceous until the Aptian – Albian, siliciclastic basin fills were characterized by transgressive fining– upward trends, with prominent first–cycle quartzose provenances that indicate strong chemical weathering in the source areas. Jurassic, Triassic, and older detrital zircon U–Pb ages suggest that the igneous and metamorphic rocks forming the basement of the Central Cordillera were the main sources. Furthermore, the presence of Early Cretaceous detrital ages between 120 and 100 Ma, together with interlayered volcanic rocks at the top of the sequence characterized by mixed arc–like, MORB, and E–MORB geochemical signatures, can be related to the evolution of an extensional arc with associated back–arc basin formation. Plutonic rocks with ca. 98 Ma crystallization ages show Nd, Sr, Hf, and O isotope evidence for the existence of thinned continental crust that may account for the dominant mantle signature. By ca. 93 Ma, the Early Cretaceous sedimentary sequences were deformed and intruded by plutonic rocks, which conversely show isotopic fingerprints characteristic of crustal signatures that can be explained by the involvement of thicker crust that promoted melt interaction with the more radiogenic host rocks.

This tectonic change from a Mariana– to an Andean–type subduction style was probably triggered by regional–scale plate kinematic reorganizations, as suggested by similar coeval tectonic scenarios along the entire South American margin, and set the conditions for the construction of the Andean chain.

 

Keywords: Cretaceous, back–arc, intra–arc, Andean Orogeny, Geochemistry.


Resumen


La evolución tectónica del borde occidental de Suramérica durante el Cretácico está marcada por el cambio de un margen convergente extensional hacia una configuración más compresiva que marca el inicio de la Orogenia Andina. En los Andes colombianos, este cambio está registrado en las rocas sedimentarias y magmáticas cretácicas de la cordillera Central. La revisión de las relaciones de campo, junto con el análisis de procedencia de rocas siliciclásticas (petrografía de areniscas y geocronología en circones detríticos de varias localidades), sugiere que durante el Cretácico Temprano hasta el Aptiano–Albiano el relleno siliciclástico de la cuenca se caracterizó por tener un carácter transgresivo granodecreciente y una composición cuarzosa con componentes de primer ciclo asociados a condiciones de meteorización intensa en el área fuente. Las edades U–Pb en circón jurásicas, triásicas y más antiguas sugieren que las fuentes principales fueron las rocas ígneas y metamórficas que conforman el basamento de la cordillera Central. Además, la presencia de edades detríticas del Cretácico Temprano entre 120 y 100 Ma, junto con la de rocas volcánicas intercaladas al tope de la secuencia que se caracterizan por una mezcla de firmas geoquímicas de arco, MORB y E–MORB, puede estar relacionada con la evolución de un arco extensional y la formación de una cuenca de retroarco. Las rocas plutónicas con edades de cristalización de ca. 98 Ma muestran evidencias isotópicas de Nd, Sr, Hf y O de afinidad mantélica que estarían asociadas a la existencia de una corteza continental adelgazada. A los ca. 93 Ma, las secuencias sedimentarias del Cretácico Temprano fueron deformadas e intruidas por rocas plutónicas, las cuales en cambio muestran características isotópicas corticales que pueden explicarse por la participación de una corteza más gruesa que promovió la interacción del fundido con las rocas caja más radiogénicas.

Este cambio tectónico de un estilo de subducción de tipo Marianas a uno de tipo andino es común en toda la margen continental suramericana y estaría asociado con reorganizaciones cinemáticas a escala de placas que marcarían el inicio de la construcción de la cadena andina.

 

Palabras clave: Cretácico, retroarco, intraarco, Orogenia Andina, geoquímica.



Abbreviations 

CLIP                                               Caribbean Large Igneous Province

E–MORB                                  Enriched mid–ocean ridge basalt

FC                                                                                              Faraday cup

DM                                                    Depleted mantle

HFSE                                             High field strength element

TDM                                               Depleted mantle model ages

HREE                                             Heavy rare earth element

ICP–AES                                    Inductively coupled plasma atomic emission spectroscopy

ICP–MS                                    Inductively coupled plasma mass spectrometry

LA–ICP–MS                      Laser ablation inductively coupled plasma mass spectrometry

LILE                                                  Large–ion lithophile element

LREE                                                Light rare earth element

MORB                                                    Mid–ocean ridge basalt

MREE                                           Middle rare earth element

TIMS                                               Thermal ionization mass spectrometry

VSMOW                                   Vienna standard mean ocean water



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