Abstract

3D seismic data, well logs, core-based lithofacies and photographs have been combined to interpret and model the depositional facies of the Mangahewa Formation of the Maui Gas Field, Taranaki Basin, New Zealand. The primary objective of the study is to generate a robust facies model for the Middle to Late Eocene (47–37 Ma) Mangahewa Formation of the field. The facies model has included eighteen depositional facies spatially distributed over the gas field. These facies are further subgrouped into three broad depositional facies associations, namely marginal marine, shallow marine and offshore environment. We have identified that marginal marine is the most dominant facies association (64%) within the model. The model visualizes estuarine and shoreface sand geobodies dominating over other facies within the model. Both geobodies comprise over 40% of all the facies interpreted in the field. The entire modeling process involves a novel stochastic approach using unique workflow that follows 3D gridding, coding of the facies classes and multiple iterations over the interpreted facies. The model therefore realistically visualizes potential facies responsible for “good”-quality reservoir sands in the Mangahewa Formation with possible retrogradation from older to younger succession.

Highlights

  • Maui Gas Field is the largest hydrocarbon-producing field of New Zealand to date, with a field size of 150 sq. km

  • The results of the facies simulations have effectively underlined the need for careful synthesis of facies complexity and inter-facies variability while evaluating depositional environments

  • The following conclusions are drawn based on the depo-facies modeling of the Mangahewa reservoir: 1 3

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Summary

Introduction

Maui Gas Field is the largest hydrocarbon-producing field of New Zealand to date, with a field size of 150 sq. km. It is considered to be a two-way dip closure anticlinal structure (Fig. 1) This field is situated in the southern region of the Taranaki Basin and is bounded from both east and west by two regional faults, Cape Egmont Fault and Whitiki Fault (Stagpoole and Nicol 2008; Laird 1993). This gas field has been producing from three main reservoir sands, namely the Mangahewa, Kaimiro and Farewell formations of the Kapuni Group (King and Thrasher 1996; Bryant et al 1994; Voggenreiter 1993). This is essential in deciphering depositional variability within the studied formation with implications for both exploration and development

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