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Abstract

G. P. Eberli, J. L. Masaferro, and J. F. ldquoRickrdquo Sarg, 2004, Seismic imaging of carbonate reservoirs and systems: AAPG Memoir 81, p. 149-168.

Copyright copy2004. The American Association of Petroleum Geologists. All rights reserved.

An Integrated Reservoir Study of the Liuhua 11-1 Field Using a High-Resolution Three-Dimensional Seismic Data Set

Christoph Heubeck,1 Kenneth Story,2 Pat Peng,3 Claire Sullivan,3 Stuart Duff4

1Department of Geosciences, Freie Universitaumlt Berlin, Berlin, Germany
2DDD Energy, Houston, Texas, U.S.A.
3BP, Houston, Texas, U.S.A.
4Independent contractor, Wellington, New Zealand

ACKNOWLEDGMENTS

This work was performed while the first four authors were with Amoco (now BP), Houston, Texas. The authors would like to thank the management of BP Amoco, Kerr McGee, and China National Offshore Oil for permission to publish this work. Shane Pelecnaty, Gregor Eberli, and Mike Grammer improved the manuscript through helpful reviews. The senior author thanks Mrs. Britta Ernst and Mrs. Martina Grundmann for help with the figures.

ABSTRACT

Liuhua 11-1 field, located in the Pearl River Mouth Basin offshore south China, consists of diagenetically altered Miocene limestone comprising a shallow-water carbonate bank. This bank forms the topmost and youngest interval of a larger, extensively karsted, buried carbonate platform. A three-dimensional (3-D) seismic survey of Liuhua field yielded a very high-resolution data set (gt200 Hz), allowing a spatial resolution less than 5 m. This data set was subsequently used to produce a reservoir model that closely linked petrophysical, log, and seismic data.

The carbonate stratigraphy suggests several subaerial exposure events that significantly modify primary stratification of the carbonate bank through diagenesis. These include freshwater leaching, burial compaction, cementation, and late diagenetic flushing of the bank. The combined diagenetic changes had three principal effects: (1) exacerbation of primary facies-dependent differences in porosity through a series of dissolution-reprecipitation steps; (2) widespread incipient carbonate collapse at or below the scale of seismic resolution; and (3) formation of numerous regionally occurring karst sinkholes of as much as 400 m diameter shortly before final drowning of the platform. Incipient collapse of the friable carbonate framework is expressed seismically by a reduction in amplitude.

Carbonate dissolution appears to be ongoing because sagging continues to affect all strata overlying the reservoir to the seafloor. Subsurface dissolution may be a result of either flushing of the carbonate platform by cold, undersaturated marine waters or may be a result of active biodegradation of the hydrocarbons along the oil-water contact and the concomitant release of acids.

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