MIND ROCK CAPITAL MRX

Brand Owner (click to sort) Address Description
MINDROCK CAPITAL MRX Cherkashin, Pavel 908 Broadway San Francisco CA 94133 San Francisco CA 94133 MIND ROCK CAPITAL MRX;Cryptocurrency trading services; Financial advice and consultancy services; Financial analysis and research services; Financial asset management; Financial consultancy; Financial consultation in the field of cryptocurrency; Financial management; Investment management; Providing investors with financial information; Venture capital fund management;
MINDROCK CAPITAL MRX i280 Ventures 908 Broadway San Francisco CA 94133 MIND ROCK CAPITAL MRX;Cryptocurrency trading services; Financial advice and consultancy services; Financial analysis and research services; Financial asset management; Financial consultancy; Financial consultation in the field of cryptocurrency; Financial management; Investment management; Providing investors with financial information; Venture capital fund management;
 

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Technical Examples
  1. A reservoir simulator first estimates rock displacement parameters (u, v, and w) representing rock movement in the x, y, and z directions. When the rock displacement parameters (u, v, w) are determined, "?x,y,z" (the 'x,y,z elongation strains') and "?xy,yz,zx" (the 'shear strains') are determined since "?x,y,z" and "?xy,yz,zx" are function of "u", "v", and "w" When "?x,y,z" and "?xy,yz,zx" are determined, "?x,y,z" (the 'elastic normal rock stress in x,y,z directions') and "?xy,yz,xz" (the 'elastic shear stress') are determined since "?x,y,z" and "?xy,yz,xz" are a function of "?x,y,z" and "?xy,yz,zx". When "?x,y,z" and "?xy,yz,xz" are determined, the rock momentum balance differential equations can be solved, since these equations are a function of "?x,y,z" and "?xy,yz,xz". When any residuals are substantially equal to zero, the estimated rock displacement parameters (u, v, and w) represent 'accurate rock displacement parameters' for the reservoir. When the rock momentum balance differential equations are solved, the rock displacement parameters (u, v, w), at an advanced time, are known. These rock displacement parameters (u, v, w) represent and characterize 'subsidence' in a seabed floor because subsidence results from rock movement; and rock movement results from withdrawal of oil or other hydrocarbon deposits or other fluids from an Earth formation. This 'abstract of the disclosure' is given for the sole purpose of allowing a patent searcher to easily determine the content of the disclosure in this application.