Hydrocarbon plumbing systems above the Sn?hvit gas field: Structural control and implications for thermogenic methane leakage in the Hammerfest Basin, SW Barents Sea

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• 作者：Ilya Ostanin^a ; ^{ostanin@gfz-potsdam.de} ; Zahie Anka^a ; Rolando di Primio^a ; Asdrú ; bal Bernal^b
• 关键词：Hydrocarbon leakage ; Snohvit gas field ; BSR ; Mega pockmarks
• 刊名：Marine and Petroleum Geology
• 出版年：2013
• 出版时间：May, 2013
• 年：2013
• 卷：43
• 期：Complete
• 页码：127-146
• 全文大小：5995 K

文摘

Based on the analysis of the high-resolution 3D seismic data from the SW Barents Sea we study the hydrocarbon plumbing system above the Sn?hvit and Albatross gas field to investigate the geo-morphological manifestation and the dynamics of leakage from the reservoir. Fluid and gas escape to the seafloor is manifested in this area as mega-pockmarks 1-2?km-wide, large pockmarks (<100?m wide) and giant pockmarks 100-300?m-wide. The size of the mega pockmarks to the south of the study area may indicate more vigorous venting, whilst the northern fluid flow regime is probably characterised by a widespread fluid and gas release. Buried mega depressions and large-to-giant pockmarks are also identified on the base Quaternary and linked to deep and shallow faults as well as to seismic pipes. A high density of buried and seafloor giant pockmarks occur above a network of faults overlying an interpreted Bottom Simulating Reflector (BSR), whose depth coincides with the estimated base of the hydrate stability zone for a thermogenically derived gas hydrate with around 90?mol % methane. Deep regional faults provide a direct route for the ascending thermogenic fluids from the reservoir, which then leaked through the shallow faults linked to seismic pipes. It is proposed that the last episodic hydrocarbon leakage from the reservoir was responsible for providing a methane source for the formation of gas hydrates. We inferred that at least two temporally and dynamically different fluid and gas venting events took place in the study area: (1) prior to late Weichselian and recorded on the Upper Regional Unconformity (URU) and (2) following the Last Glacial Maximum between ¡«17 and 16?cal ka BP and recorded on the present-day seafloor.