globalchange  > 过去全球变化的重建
DOI: 10.1306/05061413173
Scopus记录号: 2-s2.0-84916912288
论文题名:
A scaling law to characterize fault-damage zones at reservoir depths
作者: Johri M.; Zoback M.D.; Hennings P.
刊名: AAPG Bulletin
ISSN: 0149-1578
EISSN: 1558-9308
出版年: 2014
发表日期: 2014
卷: 98, 期:10
起始页码: 2057
结束页码: 2079
语种: 英语
Scopus关键词: Boreholes ; Computer simulation ; Decay (organic) ; Fracture ; Well logging ; Damage zones ; Density decay ; Density variations ; Geologic environment ; Reservoir flow ; San Andreas fault ; Second orders ; Seismic image ; Strike-slip faults ; damage mechanics ; fault geometry ; fault plane ; fault propagation ; fracture zone ; sandstone ; seismic stratigraphy ; simulation ; California ; California ; San Andreas ; United States
Scopus学科分类: Energy ; Earth and Planetary Sciences
英文摘要: We analyze fracture-density variations in subsurface fault-damage zones in two distinct geologic environments, adjacent to faults in the granitic SSC reservoir and adjacent to faults in arkosic sandstones near the San Andreas fault in central California. These damage zones are similar in terms of width, peak fracture or fault (FF) density, and the rate of FF density decay with distance from the main fault. Seismic images from the SSC reservoir exhibit a large basement master fault associated with 27 seismically resolvable second-order faults. A maximum of 5 to 6 FF/m (1.5 to 1.8 FF/ft) are observed in the 50 to 80 m (164 to 262 ft) wide damage zones associated with second-order faults that are identified in image logs from four wells. Damage zones associated with second-order faults immediately southwest of the San Andreas Fault are also interpreted using image logs from the San Andreas Fault Observatory at Depth (SAFOD) borehole. These damage zones are also 50-80 m wide (164 to 262 ft) with peak FF density of 2.5 to 6 FF/m (0.8 to 1.8 FF/ft). The FF density in damage zones observed in both the study areas is found to decay with distance according to a power law F = F0r-n. The fault constant F0 is the FF density at unit distance from the fault, which is about 10-30 FF/m (3.1-9.1 FF/ft) in the SSC reservoir and 6-17 FF/m (1.8-5.2 FF/ft) in the arkose. The decay rate n ranges from 0.68 to 1.06 in the SSC reservoir, and from 0.4 to 0.75 in the arkosic section. This quantification of damage-zone attributes can facilitate the incorporation of the geometry and properties of damage zones in reservoir flow simulation models. Copyright © 2014. The American Association of Petroleum Geologists. All rights reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84916912288&doi=10.1306%2f05061413173&partnerID=40&md5=781cd0f5f4e45fee5e65caee0d4bdf3a
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/13149
Appears in Collections:过去全球变化的重建
影响、适应和脆弱性
科学计划与规划
气候变化与战略
全球变化的国际研究计划
气候减缓与适应
气候变化事实与影响

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Johri M.,Zoback M.D.,Hennings P.. A scaling law to characterize fault-damage zones at reservoir depths[J]. AAPG Bulletin,2014-01-01,98(10)
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