Outcrop-Behind Outcrop Characterization of Thin-Bedded Turbidites for Improved Understanding of Analog Reservoirs - New Zealand and Gulf of Mexico

R. M. Slatt; G. H. Browne; G. R. Clemenceau; R. J. Davis; R. A. Young; H. Anxionnaz; R. J. Spang

doi:10.3997/2214-4609.201406604

f Outcrop-Behind Outcrop Characterization of Thin-Bedded Turbidites for Improved Understanding of Analog Reservoirs - New Zealand and Gulf of Mexico
By R. M. Slatt, G. H. Browne, G. R. Clemenceau, R. J. Davis, R. A. Young, H. Anxionnaz and R. J. Spang
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, EAGE/AAPG 3rd Research Symposium - Developing and Managing Turbidite Reservoirs, Oct 1998, cp-100-00041
ISBN: 978-94-6282-120-0
DOI: https://doi.org/10.3997/2214-4609.201406604

Abstract

A 200m high by 10km long coastal cliff section of the Late Miocene Mt. Messenger Formation, New Zealand consists of 200+ meters of mainly thick-bedded turbidite fan sands overlain by 300m of thin-bedded slope fan, levee/overbank sands/silts.

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1998-10-03

2024-04-25

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f Outcrop-Behind Outcrop Characterization of Thin-Bedded Turbidites for Improved Understanding of Analog Reservoirs - New Zealand and Gulf of Mexico

Abstract

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