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I. A. Garagash

Researcher at Russian Academy of Sciences

Publications -  41
Citations -  264

I. A. Garagash is an academic researcher from Russian Academy of Sciences. The author has contributed to research in topics: Induced seismicity & Crust. The author has an hindex of 8, co-authored 34 publications receiving 191 citations. Previous affiliations of I. A. Garagash include Shirshov Institute of Oceanology & Skolkovo Institute of Science and Technology.

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Dynamic bridging of proppant particles in a hydraulic fracture

TL;DR: In this article, a dynamic bridging criterion for the arching and bridging of spherical particles in a 3D suspension flow through a channel with plane walls is proposed. But the authors focus on the 3D motion of particles in fluid and do not consider the effects of friction on the particles.
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Geomechanical models and ionospheric variations related to strongest earthquakes and weak influence of atmospheric pressure gradients

TL;DR: In this article, the authors developed computer models for the study regions to analyze the influence of the atmospheric pressure on the stressed state of the Earth's crust, including tectonic faults of different ranks.
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The evolution of the stress state in Southern California based on the geomechanical model and current seismicity

TL;DR: In this article, a three-dimensional geomechanical model of Southern California, which includes the mountain topography, fault tectonics, and main structural boundaries (the top of the lower crust and the Moho), is developed.
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Impact of Flowback Dynamics on Fracture Conductivity

TL;DR: In this article, the authors focus on the impact of flowback dynamics on the conductivity of a single fracture in a multi-stage fractured completion and develop an integrated modeling workflow for design and optimization of the flowback operation on a multistage fractured well.
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Connection between variations of the stress-strain state of the Earth’s crust and seismic activity: The example of Southern California

TL;DR: In this article, a 3D geomechanical model of Southern California, including mountain relief, fault tectonics, and characteristic internal borders, such as the roof of the consolidated crust and Moho surface, was created.