Replication data for 'Tectonic evolution of the Indio Hills segment of the San Andreas fault in southern California'
<|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:'Field photographs and structural measurements from fieldwork along the San Andreas Fault Zone in the Indio Hills, southern California, in February-March 2017.  The text files containing the structural data include measurements of strike in the first column and dip in the second column.Transpressional uplift domains of inverted Miocene–Pliocene basin fill along the San Andreas fault zone in Coachella Valley, southern California, are characterized by fault linkage and segmentation and deformation partitioning. The Indio Hills wedge-shaped uplift block is located in between two boundary fault strands, the Indio Hills fault to the northeast and the Banning fault to the southwest, which merge to the southeast. Uplift commenced about 2.2–0.76 million years ago and involved either three separate and/or progressive fold and f' . 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" : ["Bedding surfaces","California","Faults","Fieldwork","Folds","San Andreas Fault Zone"]} <|eot_id|>
 Here is the Description of a dataset. Description:'Field photographs and structural measurements from fieldwork along the San Andreas Fault Zone in the Indio Hills, southern California, in February-March 2017.  The text files containing the structural data include measurements of strike in the first column and dip in the second column.Transpressional uplift domains of inverted Miocene–Pliocene basin fill along the San Andreas fault zone in Coachella Valley, southern California, are characterized by fault linkage and segmentation and deformation partitioning. The Indio Hills wedge-shaped uplift block is located in between two boundary fault strands, the Indio Hills fault to the northeast and the Banning fault to the southwest, which merge to the southeast. Uplift commenced about 2.2–0.76 million years ago and involved either three separate and/or progressive fold and f' . Please return only a json list of at most 3 Keywords corresponding to the Description:.
Field photographs and structural measurements from fieldwork along the San Andreas Fault Zone in the Indio Hills, southern California, in February-March 2017.  The text files containing the structural data include measurements of strike in the first column and dip in the second column.Transpressional uplift domains of inverted Miocene–Pliocene basin fill along the San Andreas fault zone in Coachella Valley, southern California, are characterized by fault linkage and segmentation and deformation partitioning. The Indio Hills wedge-shaped uplift block is located in between two boundary fault strands, the Indio Hills fault to the northeast and the Banning fault to the southwest, which merge to the southeast. Uplift commenced about 2.2–0.76 million years ago and involved either three separate and/or progressive fold and f
Bedding surfaces; California; Faults; Fieldwork; Folds; San Andreas Fault Zone