2020
DOI: 10.1016/j.gsf.2019.05.014
|View full text |Cite
|
Sign up to set email alerts
|

Effect of mineralogy on friction-dilation relationships for simulated faults: Implications for permeability evolution in caprock faults

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

2
22
0

Year Published

2021
2021
2024
2024

Publication Types

Select...
9
1

Relationship

0
10

Authors

Journals

citations
Cited by 44 publications
(24 citation statements)
references
References 60 publications
2
22
0
Order By: Relevance
“…According to the developed concept, the predicted flood volume for the study area was estimated between 634 and 825 MCM for a 100-year return period Water Supply Vol 00 No 0, 10 Uncorrected Proof (Figure 9(c)). This return period was recommended for reservoir dam design (Zhang et al 2020a(Zhang et al , 2020b. Consequently, in the 25-year return period, which is an appropriate time scale for flood diversion systems of water storage reservoirs, a flood volume of 125-164 MCM with a maximum flow of 865 m 3 /s has been obtained.…”
Section: Resultsmentioning
confidence: 99%
“…According to the developed concept, the predicted flood volume for the study area was estimated between 634 and 825 MCM for a 100-year return period Water Supply Vol 00 No 0, 10 Uncorrected Proof (Figure 9(c)). This return period was recommended for reservoir dam design (Zhang et al 2020a(Zhang et al , 2020b. Consequently, in the 25-year return period, which is an appropriate time scale for flood diversion systems of water storage reservoirs, a flood volume of 125-164 MCM with a maximum flow of 865 m 3 /s has been obtained.…”
Section: Resultsmentioning
confidence: 99%
“…The density and porosity of sample ATR-3, which is ~3 m away from the youngest fault plane of an inactive fault, are 2.56 g/cm 3 and 3.3%, respectively. Zhang et al (2020) conducted an experimental study on the behavior of fault gouge under frictional shear to examine gouge dilation, frictional strength, stability, and healing, and reported that gouge dilation decreased with increasing normal stress. Therefore, the porosity of the fault gouge along the active faults is larger than that of the fault gouge along the inactive faults because the fault gouge along active faults forms at shallower depths and has a larger dilatancy than the fault gouge along inactive faults.…”
Section: Measurement Resultsmentioning
confidence: 99%
“…Mechanical mechanisms of structural fracture growth (Olsson et al, 2004;Gale and Gomez, 2007;Zhang et al, 2020) suggests that tensile stress field occurs when the orientation of the scoring is consistent with the inclination of fracture surface [where the maximum principal stress (σ 1 ) is vertical and the intermediate principal stress (σ 2 ) and the minimum principal stress (σ 3 ) are horizontal], and it is consistent with the tensile stress field at the late Paleogene of Nanpu Sag (Tong et al, 2013), where NE-SW horizontal compression and NW-SE tensile stress developed NE-SW direction shear fractures. Strike-slip tectonic stress occurs when the scoring shares the same orientation with fracture surface (where the σ 2 is vertical, the σ 1 and σ 3 are horizontal).…”
Section: Discussionmentioning
confidence: 99%