Replication Data for: Correlation between tectonic stress regimes and methane seepage on the west-Svalbard margin
<|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:'Abstract: Methane seepage occurs across the west-Svalbard margin at water depths ranging from  1000 m in regions just a few kilometres away from the mid-ocean ridges in the Fram Strait. The mechanisms controlling seepage remain elusive. The Vestnesa sedimentary ridge, located on oceanic crust at 1000-1700 m water depth, hosts a perennial gas hydrate and associated free gas system. The restricted occurrence of acoustic flares to the eastern segment of the sedimentary ridge, despite the presence of pockmarks along the entire ridge, indicates a spatial variation in seepage activity. This variation coincides with a change in the faulting pattern as well as in the characteristics of fluid flow features. Due to the position of the Vestnesa ridge with respect to the Molloy and Knipovich mid-ocea' . 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" : ["Arctic","faults","Fram Strait","gas hydrates","greenhouse gases","marine seepage","methane","P-Cable seismics","seepage","seismics","tectonic stress","tectonic stress","Western Svalbard","Western Svalbard margin"]} <|eot_id|>
 Here is the Description of a dataset. Description:'Abstract: Methane seepage occurs across the west-Svalbard margin at water depths ranging from  1000 m in regions just a few kilometres away from the mid-ocean ridges in the Fram Strait. The mechanisms controlling seepage remain elusive. The Vestnesa sedimentary ridge, located on oceanic crust at 1000-1700 m water depth, hosts a perennial gas hydrate and associated free gas system. The restricted occurrence of acoustic flares to the eastern segment of the sedimentary ridge, despite the presence of pockmarks along the entire ridge, indicates a spatial variation in seepage activity. This variation coincides with a change in the faulting pattern as well as in the characteristics of fluid flow features. Due to the position of the Vestnesa ridge with respect to the Molloy and Knipovich mid-ocea' . Please return only a json list of at most 3 Keywords corresponding to the Description:.
Abstract: Methane seepage occurs across the west-Svalbard margin at water depths ranging from  1000 m in regions just a few kilometres away from the mid-ocean ridges in the Fram Strait. The mechanisms controlling seepage remain elusive. The Vestnesa sedimentary ridge, located on oceanic crust at 1000-1700 m water depth, hosts a perennial gas hydrate and associated free gas system. The restricted occurrence of acoustic flares to the eastern segment of the sedimentary ridge, despite the presence of pockmarks along the entire ridge, indicates a spatial variation in seepage activity. This variation coincides with a change in the faulting pattern as well as in the characteristics of fluid flow features. Due to the position of the Vestnesa ridge with respect to the Molloy and Knipovich mid-ocea
Arctic; faults; Fram Strait; gas hydrates; greenhouse gases; marine seepage; methane; P-Cable seismics; seepage; seismics; tectonic stress; tectonic stress; Western Svalbard; Western Svalbard margin