In-situ stress measurement in the shallow basement of the Shanghai area and its structural geological significance

ZHANG Hao; SHI Gang; WU Hong; SHAO Lei; WANG Qian

doi:10.12090/j.issn.1006-6616.2020.26.04.051

Volume 26 Issue 4

Aug. 2020

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Article Navigation > Journal of Geomechanics > 2020 > 26(4): 583-594

ZHANG Hao, SHI Gang, WU Hong, et al., 2020. In-situ stress measurement in the shallow basement of the Shanghai area and its structural geological significance. Journal of Geomechanics, 26 (4): 583-594. DOI: 10.12090/j.issn.1006-6616.2020.26.04.051

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In-situ stress measurement in the shallow basement of the Shanghai area and its structural geological significance

doi: 10.12090/j.issn.1006-6616.2020.26.04.051

ZHANG Hao^{1, 2
,},
SHI Gang^{2
,
,},
WU Hong²,
SHAO Lei¹,
WANG Qian²

1.
State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
2.
Shanghai Institute of Geological Engineering Exploration, Shanghai 200072, China

More Information

Received: 2020-03-07
Revised: 2020-05-12
Published: 2020-08-01

Abstract

Abstract

By the hydraulic fracturing method and the ultrasonic imaging logging method, in-situ stress measurement was carried out in the shallow basement (180 m depth range) of the Shanghai area. The measurement results show that the maximum horizontal principal stress is between 9.54~12.91 MPa, and the minimum principal stress is between 5.41~6.96 MPa. The maximum horizontal principal stress direction is NW42°-62°, the dominant orientation is NW, and the stress structure is S_H > S_h > S_v, which reflects the characteristics of the regional structural stress field. Based on the spatial distribution of the internal fractures in the area and the in-situ stress measurement results, the NE faults are prone to compressive or compression-torsional reverse faulting and the faults are relatively stable, while the NW faults are prone to tensile or tension-torsional positive faulting, which is still worthy of attention under the current relatively high stress level. At the same time, the in-situ stress measurement results may have guiding significance for the study of the structural boundary trend (the Jiangshan-Shaoxing fault) in this area.
- in-situ stress,
- hydraulic fracturing,
- ultrasonic imaging logging,
- fault activity,
- regional tectonic dynamic background

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In-situ stress measurement in the shallow basement of the Shanghai area and its structural geological significance

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In-situ stress measurement in the shallow basement of the Shanghai area and its structural geological significance

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