深水碎屑岩区注砂——运移路径、侵入圈闭和储层特征

A. Hurst, D. Duranti, M. Huuse, J. Cartwright
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深水碎屑岩区注砂:运移路径、侵入圈闭及储层特征HURST *1 D. DURANTI 1 M. HUUSE 2 AND J. CARTWRIGHT 2 1阿伯丁大学地质与石油地质系阿伯丁AB24 3UE UK (a.hurst@abdn.ac.uk d.duranti@abdn.ac.uk) 2 3DLab地球海洋与行星科学系英国威尔士卡迪夫大学(m.huuse@earth.cf.ac.uk joe@ocean.cf.ac.uk)注砂越来越普遍地与深水碎屑储层联系在一起。它们改变了储层砂岩的内部和外部几何形状,有时形成具有商业意义的圈闭,这些圈闭可分为侵入型或挤压型。注砂形式
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Sand Injectites in Deep-Water Clastic Plays – Migration Paths, Intrusive Traps and Reservoir Characterisation
A025 SAND INJECTITES IN DEEP-WATER CLASTIC PLAYS: MIGRATION PATHS INTRUSIVE TRAPS AND RESERVOIR CHARACTERISATION Abstract 1 A. HURST *1 D. DURANTI 1 M. HUUSE 2 AND J. CARTWRIGHT 2 1 Department of Geology and Petroleum Geology University of Aberdeen Aberdeen AB24 3UE UK (a.hurst@abdn.ac.uk d.duranti@abdn.ac.uk) 2 3DLab Department of Earth Ocean and Planetary Sciences Cardiff University Wales UK (m.huuse@earth.cf.ac.uk joe@ocean.cf.ac.uk) Sand injectites are increasingly commonly identified in association with deep-water clastic reservoirs. They modify the internal and external geometry of reservoir sandstones and sometime form commercially significant traps which may be classed as intrusive or extrusive traps. Sand injectites form
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