Turbidite channel reservoirs - Key elements in facies prediction and effective development

被引:436
作者
Mayall, Mike
Jones, Ed
Casey, Mick
机构
[1] BP Int Ltd, Sunbury On Thames TW16 7LN, Middx, England
[2] BP Explorat & Prod, Cairo, Egypt
[3] BP Amoco Explorat, Houston, TX 77253 USA
关键词
turbidite system; channel; reservoir;
D O I
10.1016/j.marpetgeo.2006.08.001
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Turbidite channels are important but frequently complex reservoirs in the exploration, appraisal and development of deep-water facies. Over the last 10 years in particular, high-resolution seismic data and extensive outcrop studies have increased our knowledge of the complexity of these sedimentary bodies. Such is their variability and complexity that developing and applying single or even multiple depositional models has limited applicability. Instead, we recognise an alternative approach to help rapidly evaluate turbidite channel reservoirs. The paper mainly concerns the evaluation of large erosionally confined 3rd-order channels, typically 1-3 km wide and 50-200 m thick. Each channel is unique but each generally has four recurring elements namely, the sinuosity, the facies, repeated cutting and filling and the stacking patterns. Several different styles of sinuosity can be identified, each having different implications for sand distribution. Four main facies can often be recognised on seismic, calibrated by cores and logs; a basal lag, slump/debris flows, high net:gross stacked channels and low N:G channel levees. Most channels contain all of these facies but in widely varying proportions. Repeated cutting and filling is a feature of just about every channel studied. The process has major implications for reservoir and non-reservoir distribution. The stacking patterns of the 4/5th-order channels within the 3rd-order channel can have a critical impact on facies and heterogeneity distribution and can strongly influence well design and even potentially the development concept. This paper discusses the impact of each of these elements on exploration, appraisal and development issues. (c) 2006 Elsevier Ltd. All rights reserved.
引用
收藏
页码:821 / 841
页数:21
相关论文
共 72 条
[31]   Downstream evolution of turbiditic channel complexes in the Pab Range outcrops (Maastrichtian, Pakistan) [J].
Eschard, R ;
Albouy, E ;
Deschamps, R ;
Euzen, T ;
Ayub, A .
MARINE AND PETROLEUM GEOLOGY, 2003, 20 (6-8) :691-710
[32]   3D seismic images of a low-sinuosity slope channel and related depositional lobe (West Africa deep-offshore) [J].
Fonnesu, F .
MARINE AND PETROLEUM GEOLOGY, 2003, 20 (6-8) :615-629
[33]  
Fugitt D. S, 2000, DEEP WATER RESERVOIR, P389
[34]  
Gammon P. R., 2007, DEEP WATER RESERVOIR, V56, P102
[35]   Stratigraphic process-response model for submarine channels and related features from studies of Permian Brushy Canyon outcrops, West Texas [J].
Gardner, MH ;
Borer, JA ;
Melick, JJ ;
Mavilla, N ;
Dechesne, M ;
Wagerle, RN .
MARINE AND PETROLEUM GEOLOGY, 2003, 20 (6-8) :757-787
[36]  
Gardner MH, 2000, AAPG MEMOIR, V72, P195
[37]   Evolving turbidite systems on a deforming basin floor, Tabernas, SE Spain [J].
Haughton, PDW .
SEDIMENTOLOGY, 2000, 47 (03) :497-518
[38]   Facies architecture of a submarine fan channel-levee complex: The Juniper Ridge Conglomerate, Coalinga, California [J].
Hickson, TA ;
Lowe, DR .
SEDIMENTOLOGY, 2002, 49 (02) :335-362
[39]  
HUMPHREYS NV, 1999, TECHNOLOGY APPL ENAB
[40]   Anatomy, geometry and sequence stratigraphy of basin floor to slope turbidite systems, Tanqua Karoo, South Africa [J].
Johnson, SD ;
Flint, S ;
Hinds, D ;
Wickens, HD .
SEDIMENTOLOGY, 2001, 48 (05) :987-+