Constraining sub-seismic deep-water stratal elements with electrofacies analysis; A case study from the Upper Cretaceous of the Måløy Slope, offshore Norway

Abstract

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Evolution of a sand-rich submarine channel–lobe system, and the impact of mass-transport and transitional-flow deposits on reservoir heterogeneity: Magnus Field, Northern North Sea

“…Recognition of sub-seismic sealing MTDs should be undertaken through the integration of multiple datasets, particularly pressure measurements which provide a valuable dynamic validation of hydraulic sealing. For example in the Måløy Slope, offshore Norway, sub-seismic debrites and slumped units can be identified by integration of well-logs through electro-facies analysis (Prélat et al 2015). The Buzzard Field, in the Central North Sea, shows how intra-reservoir mud-prone slump units were initially predicted to be sealing, however, during production bounding reservoir units were found to be in pressure communication (Ray et al 2010).…”

Karakteristik Sedimen Palung Laut Sulawesi (Core Sta12) Berdasarkan Hasil Pengamatan Megaskopis Dan Sifat Fisika Dari Pengukuran Multi-Sensor Core Logger (Mscl)

“…Cepat rambat gelombang P ini diduga terkait densitas sedimen yang lebih tinggi pada sedimen yang lebih gelap dibandingkan sedimen yang lebih cerah. Hal ini sangat sesuai dengan studi terdahulu terkait hubungan antara densitas dan kecepatan transmisi gelombang P (Prélat et al, 2015).…”