SPLIT ROCK

Brand	Owner (click to sort)	Address	Description
SPLITROCK	SPLITROCK SERVICES, INC.	8665 New Trails Dr., Suite 200 The Woodlands TX 77381	SPLIT ROCK;providing multiple-user access to a global computer information network for the transfer and dissemination of a wide range of information; and providing access time to computer data bases/web sites/home pages of others by means of a global computer network;The stippling in the drawing indicates shading and is not a feature of a mark.;
SPLITROCK	SPLITROCK SERVICES INC.	8665 NEW TRAILS DRIVE, SUITE 200 THE WOODLAND TX 77381	SPLIT ROCK;providing multiple-user access to a global computer information network for the transfer and dissemination of a wide range of information; and providing access time to computer data bases/web sites/home pages of others by means of a global computer network;
SPLITROCK	SPLITROCK SERVICES, INC.	8665 New Trails Dr., Suite 200 The Woodlands TX 77381	SPLIT ROCK;providing multiple-user access to a global computer information network for the transfer and dissemination of a wide range of information; and providing access time to computer data bases/web sites/home pages of others by means of a global computer network;
SPLITROCK	Given, Lachlan	136 10th Avenue, Apt. 1 New York NY 10011	SPLIT ROCK;Carbonated and non-carbonated drinking water, mineral water, soft drinks, carbonated and non-carbonated flavored water, fruit-based drinks, fruit juices;
	Where the owner name is not linked, that owner no longer owns the brand

Technical Examples

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.