IP Library Granted Patent US 7,663,970
Granted Patent B2
US 7,663,970 · App. 11/522,183 · Granted Feb 16, 2010

Method for passive seismic emission tomography

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Quick Facts
Patent No.
US 7,663,970
App. No.
11/522,183
Granted
Feb 16, 2010
Kind
B2
Abstract

A method for seismic event mapping includes transforming seismic signals recorded at selected positions into a domain of possible spatial positions of a source of seismic events. An origin in spatial position and time of at least one seismic event is determined from space and time distribution of at least one attribute of the transformed seismic data.

Claims (31)

1. A method for seismic event mapping, comprising:

transforming seismic signals recorded from seismic sensors deployed at selected positions proximate a volume of the Earth's subsurface to be evaluated, the signals being at least one of electrical and optical signals representing measured seismic amplitude with respect to time resulting from seismic events occurring in the volume of the subsurface, the signals conducted to a recording unit for recording, into a domain of possible spatial positions of a source of seismic events; and

determining an origin in spatial position and time of at least one seismic event in the subsurface volume from space and time distribution of at least one attribute of the transformed seismic data, the determining the origin in including identifying events in the transformed signals that have characteristics corresponding to seismic events, and determining the origin when selected ones of the events meet predetermined space and time distribution criteria.

2. The method of claim 1 wherein the transforming is performed using a model of velocity of Earth formations in a volume of the Earth's subsurface associated with the domain.

3. The method of claim 1 wherein the predetermined characteristics comprise amplitude.

4. The method of claim 1 wherein the events are identified by:

selecting amplitude features in the transformed signals that exceed a selected threshold;

sorting the features by amplitude;

identifying corresponding features in geometrically proximate transformed signals;

aggregating the corresponding features; and

estimating a geometric center of the aggregated corresponding features.

5. The method of claim 4 wherein the estimating a geometric center comprises selecting a geometric position corresponding to the one of the features having a maximum amplitude.

6. The method of claim 4 wherein the estimating a geometric center comprises estimating a center of a mean of a distribution of the features.

7. The method of claim 1 wherein the events are identified by calculating a weighted sum of a characteristic of the transformed recorded signals.

8. The method of claim 1 wherein the selected positions are proximate the Earth's surface.

9. A method for monitoring fracture fluid front movement in the Earth's subsurface, comprising:

recording seismic signals at selected positions proximate a wellbore during pumping of fracturing fluid into the wellbore;

transforming the recorded signals into a domain of possible spatial positions of a source of seismic events; and

determining at least one origin in spatial position and time of at least one seismic event associated with movement of the fracturing fluid front from space and time distribution of at least one attribute of the transformed seismic signals, the determining the origin in including identifying events in the transformed signals that have characteristics corresponding to seismic events, and determining the origin when selected ones of the identified events meet predetermined space and time distribution criteria.

10. The method of claim 9 wherein the transforming is performed using a model of velocity of Earth formations in a volume of the Earth's subsurface associated with the domain.

11. The method of claim 9 wherein the predetermined characteristics comprise amplitude.

12. The method of claim 9 wherein the events are identified by:

selecting amplitude features in the transformed signals that exceed a selected threshold;

sorting the features by amplitude;

identifying corresponding features in geometrically proximate transformed signals;

aggregating the corresponding features; and

estimating a geometric center of the aggregated corresponding features.

13. The method of claim 12 wherein the estimating a geometric center comprises selecting a geometric position corresponding to the one of the features having a maximum amplitude.

14. The method of claim 12 wherein the estimating a geometric center comprises estimating a center of a mean of a distribution of the features.

15. The method of claim 9 wherein the events are identified by calculating a weighted sum of a characteristic of the transformed recorded signals.

16. The method of claim 9 wherein the selected positions are proximate the Earth's surface.

Assignments (5)
CORRECTIVE ASSIGNMENT TO CORRECT THE UNDERLYING DOCUMENT PREVIOUSLY RECORDED AT REEL: 051289 FRAME: 0353. ASSIGNOR(S) HEREBY CONFIRMS THE SECURITY INTEREST. Recorded Dec 18, 2019
From: MICROSEISMIC, INC.
To: SILICON VALLEY BANK
Reel/Frame 051344/0376 →
SECURITY INTEREST Recorded Dec 16, 2019
From: MICROSEISMIC, INC.
To: SILICON VALLEY BANK
Reel/Frame 051289/0353 →
FIRST AMENDMENT TO INTELLECTUAL PROPERTY SECURITY AGREEMENT Recorded Jul 20, 2018
From: MICROSEISMIC, INC.
To: SILICON VALLEY BANK
Reel/Frame 046596/0361 →
RELEASE OF SECURITY INTEREST Recorded Apr 12, 2017
From: PNC BANK, NATIONAL ASSOCIATION
To: MICROSEISMIC, INC.
Reel/Frame 041988/0238 →
SECURITY INTEREST Recorded Apr 10, 2017
From: MICROSEISMIC, INC.
To: SILICON VALLEY BANK
Reel/Frame 041941/0616 →