Testing the `terrane-boundary' concept and geodynamics in the Neoarchean: A case study of the stratigraphy from the West and East Laverton Greenstone Belts
<|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:'PhD thesis abstract:Archean (>2.5 billion years: Ga) cratons consist of numerous crustal blocks that are separated by crustal-scale structures. Knowledge of how these crustal blocks came to be in their current configuration has implications for geodynamic models, links to other cratons and mineral exploration. Largely on account of poor 3D exposure, the study of Archean structures is insufficient to fully address questions of their origin. The Hootanui Shear Zone (HSZ) in the Eastern Goldfields Superterrane (Yilgarn Craton, Western Australia) is ascribed a variety of origins, including a suture between two tectonic plates, an intra-arc structure, or as the margin of a rift. In this study the well-preserved volcano-sedimentary sequences from either side of the HSZ (the West and East Laverton Greenstone belts), are characterised from fi' . 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" : ["Archean","East Goldfields Superterrane","EGST","geochemistry","geology","greenstone correlations","intracratonic rift","Lu-Hf geochronology","mineral exploration","rift margin","stratigraphy","terrane boundary","U-Pb geochronology","Yilgarn Craton"]} <|eot_id|>
 Here is the Description of a dataset. Description:'PhD thesis abstract:Archean (>2.5 billion years: Ga) cratons consist of numerous crustal blocks that are separated by crustal-scale structures. Knowledge of how these crustal blocks came to be in their current configuration has implications for geodynamic models, links to other cratons and mineral exploration. Largely on account of poor 3D exposure, the study of Archean structures is insufficient to fully address questions of their origin. The Hootanui Shear Zone (HSZ) in the Eastern Goldfields Superterrane (Yilgarn Craton, Western Australia) is ascribed a variety of origins, including a suture between two tectonic plates, an intra-arc structure, or as the margin of a rift. In this study the well-preserved volcano-sedimentary sequences from either side of the HSZ (the West and East Laverton Greenstone belts), are characterised from fi' . Please return only a json list of at most 3 Keywords corresponding to the Description:.
PhD thesis abstract:Archean (>2.5 billion years: Ga) cratons consist of numerous crustal blocks that are separated by crustal-scale structures. Knowledge of how these crustal blocks came to be in their current configuration has implications for geodynamic models, links to other cratons and mineral exploration. Largely on account of poor 3D exposure, the study of Archean structures is insufficient to fully address questions of their origin. The Hootanui Shear Zone (HSZ) in the Eastern Goldfields Superterrane (Yilgarn Craton, Western Australia) is ascribed a variety of origins, including a suture between two tectonic plates, an intra-arc structure, or as the margin of a rift. In this study the well-preserved volcano-sedimentary sequences from either side of the HSZ (the West and East Laverton Greenstone belts), are characterised from fi
Archean; East Goldfields Superterrane; EGST; geochemistry; geology; greenstone correlations; intracratonic rift; Lu-Hf geochronology; mineral exploration; rift margin; stratigraphy; terrane boundary; U-Pb geochronology; Yilgarn Craton