Replication Data for: Geological controls on fluid flow and gas hydrate pingo development on the Barents Sea 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:In 2014, the discovery of seafloor mounds leaking methane gas into the water columnin the northwestern Barents Sea became the first to document the existence of non-permafrost related gas hydrate pingos (GHP) on the Eurasian Arctic shelf. The discovered site is given attention because the gas hydrates occur close to the upper limit of the gas hydrate stability, thus may be vulnerable to climatic forcing. In addition, this site lies on the regional Hornsund Fault Zone marking a transition between the oceanic and continental crust. The Hornsund Fault Zone is known to coincide with an extensive seafloor gas seepage area; however, until now lack of seismic data prevented connecting deep structural elements to shallow seepages. Here we use high-resolution P-Cable 3D seismic data to study the subsurface architecture of GHPs' . 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" : ["Barents Sea","Fluid flow","Gas hydrate pingos","Hornsund Fault Zone","Seismic"]} <|eot_id|>
 Here is the Description of a dataset. Description:'Abstract:In 2014, the discovery of seafloor mounds leaking methane gas into the water columnin the northwestern Barents Sea became the first to document the existence of non-permafrost related gas hydrate pingos (GHP) on the Eurasian Arctic shelf. The discovered site is given attention because the gas hydrates occur close to the upper limit of the gas hydrate stability, thus may be vulnerable to climatic forcing. In addition, this site lies on the regional Hornsund Fault Zone marking a transition between the oceanic and continental crust. The Hornsund Fault Zone is known to coincide with an extensive seafloor gas seepage area; however, until now lack of seismic data prevented connecting deep structural elements to shallow seepages. Here we use high-resolution P-Cable 3D seismic data to study the subsurface architecture of GHPs' . Please return only a json list of at most 3 Keywords corresponding to the Description:.
Abstract:In 2014, the discovery of seafloor mounds leaking methane gas into the water columnin the northwestern Barents Sea became the first to document the existence of non-permafrost related gas hydrate pingos (GHP) on the Eurasian Arctic shelf. The discovered site is given attention because the gas hydrates occur close to the upper limit of the gas hydrate stability, thus may be vulnerable to climatic forcing. In addition, this site lies on the regional Hornsund Fault Zone marking a transition between the oceanic and continental crust. The Hornsund Fault Zone is known to coincide with an extensive seafloor gas seepage area; however, until now lack of seismic data prevented connecting deep structural elements to shallow seepages. Here we use high-resolution P-Cable 3D seismic data to study the subsurface architecture of GHPs
Barents Sea; Fluid flow; Gas hydrate pingos; Hornsund Fault Zone; Seismic