The morphologies and genesis of mega-pockmarks near the Xisha Uplift, South China Sea

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• 作者：Qiliang Sun^a ; ^b ; ^{sunqiliang@qdio.ac.cn} ; Shiguo Wu^a ; Martin Hovland^c ; ^d ; Peng Luo^e ; Yintao Lu^f ; Tailai Qu^g
• 关键词：Mega-pockmarks ; Bottom currents ; Fluid flow ; Crescentic pockmarks ; South China sea
• 刊名：Marine and Petroleum Geology
• 出版年：2011
• 出版时间：June 2011
• 年：2011
• 卷：28
• 期：6
• 页码：1146-1156
• 全文大小：4140 K

文摘

Pockmarks are normally regarded to be manifestations of fluids escape through the seabed. Kilometer-wide depressions, here called mega-pockmarks occur as widespread features near the Xisha Uplift, northern South China Sea. Most of the pockmarks observed in this area are multi-kilometers and much larger than normal-pockmarks reported worldwide. The maximum diameter observed is 3210 m and the maximum depth observed is 165.2 m based on multibeam data and 2D seismic data. The pockmarks are circular, elliptical and crescentic in plan view. Seismic profiles show that the genesis of pockmarks is related to fluid (gas and/or pore water) escape. According to the fluids pathways, the pockmarks fall into four types: (1) gas chimney-related; (2) depositional boundary-related; (3) gas chimney and inclined structure (fault)-related; (4) inclined structure-related. Bottom currents are strong and complex in the study area. The multibeam data and seismic profiles indicate that they may play an important role on extension, maintenance and shaping of pockmarks. The research of the study area is in its initial stage, and the identification of these features as indicators of fluid flow is probably useful for hydrocarbon exploration.