Understanding present-day stress in the onshore Canning Basin of Western Australia

被引:5
作者
Bailey, A. H. E. [1 ]
Jarrett, A. J. M. [1 ]
Tenthorey, E. [1 ]
Henson, P. A. [1 ]
机构
[1] Geosci Australia, Symonston, ACT, Australia
关键词
Canning Basin; Exploring for the Future; in situ stress; present-day stress; mechanical earth models; image logs; wellbore failure; poroelastic stresses; rock properties;
D O I
10.1080/08120099.2021.1879265
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Western Australia's Canning Basin is an underexplored prospective basin with proven petroleum systems and small-scale production. Recently, several formations within deeper depocentres have been investigated for unconventional hydrocarbon resources. Modern petroleum resource evaluation generally depends on an understanding of local and regional stresses that are a primary control over the formation and propagation of induced fractures. There are significant gaps in our understanding of these factors within the Canning Basin. This study characterises the regional stress regime of the onshore Canning Basin and presents modelled present-day stress, allowing for the identification of significant stress heterogeneity and natural fracture barriers. Interpretation of wireline data reveals a present-day state of stress with variation in magnitude and faulting-type. An approximately northeast-southwest regional present-day maximum horizontal stress orientation is interpreted, which is in broad agreement with the Australian Stress Map and previously published data. One-dimensional mechanical earth models, constructed for intervals from 15 Canning Basin wells, highlight the relationship between lithology and stress. Significant changes in stress within and between lithological units, owing to the existence of discrete mechanical units forming numerous inter- and intra-formational stress boundaries, likely to act as natural barriers to fracture propagation, particularly within those units currently targeted for their unconventional resource potential, are interpreted. A strike-slip faulting stress regime is interpreted broadly through the basin. However, when analysed in detail there are three distinct stress zones identified: (1) a transitional reverse- to strike-slip faulting stress regime in the top similar to 1 km, (2) a strike-slip faulting stress regime from similar to 1 km to similar to 3.0 km and (3) a transitional strike-slip to normal faulting regime at depths greater than similar to 3.0 km. This study is a component of the Australian Government's Exploring for the Future initiative, which focusses on gathering new data and information about northern Australia's resource potential.
引用
收藏
页码:818 / 838
页数:21
相关论文
共 95 条
[1]  
Anderson E.M., 1951, DYNAMICS FAULTING DI
[2]  
[Anonymous], 2017, AGES 2017
[3]  
[Anonymous], 1994, SEDIMENTARY BASINS W
[4]  
[Anonymous], 2003, GEOLOGICAL SOC AM, DOI DOI 10.1130/0-8137-2372-8.49
[5]  
[Anonymous], 2015, ANN GEOSC EXPL SEM A, P48
[6]  
Arthur J.D., 2009, GULF COAST ASS GEOLO, V59, P49
[7]  
Backhouse J., 2020, 207 GEOL SURV W AUST
[8]  
Bailey A., 2018, ASEG EXT ABSTR, V2018, P1, DOI [10.1071/ASEG2018abM1_2B, DOI 10.1071/ASEG2018ABM1_2B]
[9]  
Bailey A. H. E., 2019, The APPEA Journal, V59, DOI [10.1071/aj18259, DOI 10.1071/AJ18259]
[10]  
BAUMGARTNER J, 1989, INT J ROCK MECH MIN, V26