2022
DOI: 10.1007/s40948-022-00401-6
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Modeling of in-situ horizontal stresses and orientation of maximum horizhontal stress in the gas hydrate-bearing sediments of the Mahanadi offshore basin, India

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Cited by 9 publications
(2 citation statements)
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“…River confluences are where rivers meet and are therefore fundamental components of natural channel drainage networks (Shukla et al, 2022a). The river confluence is an environment with continuous changes in the flow structure such as speed, direction and flow rate (Best & Rhoads, 2008;Yuan et al, 2022); in the composition of sediments and nutrients (Nazari-Giglou et al, 2016;Yu et al, 2020); and in the morphology of the receptor channel (Best & Roy, 1991;Sukhodolov et al, 2023).…”
Section: Introductionmentioning
confidence: 99%
“…River confluences are where rivers meet and are therefore fundamental components of natural channel drainage networks (Shukla et al, 2022a). The river confluence is an environment with continuous changes in the flow structure such as speed, direction and flow rate (Best & Rhoads, 2008;Yuan et al, 2022); in the composition of sediments and nutrients (Nazari-Giglou et al, 2016;Yu et al, 2020); and in the morphology of the receptor channel (Best & Roy, 1991;Sukhodolov et al, 2023).…”
Section: Introductionmentioning
confidence: 99%
“…When the distance between the tested fractures is greater than 50 m, a stress gradient value needs to be provided [10]. At present, due to limited measured data and geological information, studies typically use numerical simulation technology to invert the distribution characteristic of 3-D in situ stress fields for the entire research area [14][15][16]. However, the accuracy of the in situ stress field obtained using this method depends not only on the reliability and representativeness of the in situ stress testing data but also on numerous factors such as numerical models, boundary conditions, and geological parameters [17].…”
Section: Introductionmentioning
confidence: 99%