Replication Data for: Cenozoic stages of forearc evolution following the accretion of a sliver from the Late Cretaceous-Caribbean Large Igneous Province (CLIP): SW Ecuador-NW Peru
<|begin_of_text|><|start_header_id|>system<|end_header_id|> You are a research archivist expert in dataset metadata. Answer the question truthfully.  <|eot_id|><|start_header_id|>user<|end_header_id|> Here is the Description of a dataset. Description:'The dataset include 2D seismic profiles and well log data from the Gulf of Guayaquil-Tumbes basin, SW Ecuador-NW Peru, used in the article: Cenozoic stages of forearc evolution following the accretion of a sliver from the Late Cretaceous-Caribbean Large Igneous Province (CLIP): SW Ecuador-NW Peru, 'Article accepted'.The SW Ecuador-NW Peru forearc region is the southernmost location, where the Caribbean Large Igneous Province (CLIP) interacted with the South American margin since the Late Cretaceous. The accretion of the CLIP to the margin led to the entrapment of the North Andean crustal Sliver, conforming the underlying basement of the forearc region in Ecuador, whereas in NW Peru, forearc depocenters involve rocks of continental affinity. Many existing tectonic reconstructions have treated these two areas independently, largely ba' . Please return only a json list of at most 3 Keywords corresponding to the Description:.<|eot_id|><|start_header_id|>assistant<|end_header_id|> {"Answer" : ["Caribbean Large Igneous Province","Forearc","North Andean Sliver"]} <|eot_id|>
 Here is the Description of a dataset. Description:'The dataset include 2D seismic profiles and well log data from the Gulf of Guayaquil-Tumbes basin, SW Ecuador-NW Peru, used in the article: Cenozoic stages of forearc evolution following the accretion of a sliver from the Late Cretaceous-Caribbean Large Igneous Province (CLIP): SW Ecuador-NW Peru, 'Article accepted'.The SW Ecuador-NW Peru forearc region is the southernmost location, where the Caribbean Large Igneous Province (CLIP) interacted with the South American margin since the Late Cretaceous. The accretion of the CLIP to the margin led to the entrapment of the North Andean crustal Sliver, conforming the underlying basement of the forearc region in Ecuador, whereas in NW Peru, forearc depocenters involve rocks of continental affinity. Many existing tectonic reconstructions have treated these two areas independently, largely ba' . Please return only a json list of at most 3 Keywords corresponding to the Description:.
The dataset include 2D seismic profiles and well log data from the Gulf of Guayaquil-Tumbes basin, SW Ecuador-NW Peru, used in the article: Cenozoic stages of forearc evolution following the accretion of a sliver from the Late Cretaceous-Caribbean Large Igneous Province (CLIP): SW Ecuador-NW Peru, 'Article accepted'.The SW Ecuador-NW Peru forearc region is the southernmost location, where the Caribbean Large Igneous Province (CLIP) interacted with the South American margin since the Late Cretaceous. The accretion of the CLIP to the margin led to the entrapment of the North Andean crustal Sliver, conforming the underlying basement of the forearc region in Ecuador, whereas in NW Peru, forearc depocenters involve rocks of continental affinity. Many existing tectonic reconstructions have treated these two areas independently, largely ba
Caribbean Large Igneous Province; Forearc; North Andean Sliver