Mapping Hydrocarbons by Integrating Seismic With Electromagnetic and Gravity Attributes

Electromagnetic attributes have been used extensively for interpreting marine controlled-source electromagnetic (CSEM) data.

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Fig. 2—CSEM receivers (white symbols) on the depth map of carbonates as interpreted from seismic data (warm colors indicate shallower depth). The black lines represent two examples of CSEM towing directions, CSEM 01 (southwest/northeast) and CSEM 02 (southeast/northwest).

Electromagnetic attributes have been used extensively for interpreting marine controlled-source electromagnetic (CSEM) data. One of the basic attributes is called NAR (normalized-anomalous-amplitude response). Combining NAR and CSEM asymmetry represents a relatively simple way to use the benefits of both attributes jointly. This integrated approach, based on seismic data combined with electromagnetic and gravity attributes, has been applied in a complex exploration area in the Barents Sea.

Introduction

Inversion of geophysical data measured at surface represents a quantitative approach for estimating physical properties of hydrocarbon reservoirs and obtaining information about background geology (faults, structural trends, and lateral geological variations). This approach generally is based on the minimization of an objective function including the misfit between observed and predicted responses plus a regularization function. Inversion methods generally require long computation times and extensive use of parallel-computing resources.

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