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Depth-varying-to-density earth crust extension coefficient thermal calibration gravity anomaly retrieval method

A depth-variable density and gravity anomaly technology, applied in seismic signal processing and other directions, can solve problems such as crustal density changes and gravity interpretation distortion

Inactive Publication Date: 2015-03-25
SOUTH CHINA SEA INST OF OCEANOLOGY - CHINESE ACAD OF SCI
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  • Abstract
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  • Claims
  • Application Information

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Problems solved by technology

However, thermal perturbations in the lithosphere will cause changes in the crustal density, which will distort the gravitational interpretation and should be corrected
[0011] So far, there is no report on the work of the thermally corrected gravity inversion method for the crustal extension coefficient with variable density at depth

Method used

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  • Depth-varying-to-density earth crust extension coefficient thermal calibration gravity anomaly retrieval method
  • Depth-varying-to-density earth crust extension coefficient thermal calibration gravity anomaly retrieval method
  • Depth-varying-to-density earth crust extension coefficient thermal calibration gravity anomaly retrieval method

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Embodiment 1

[0060] refer to figure 1 , the depth-variable-density crustal extension coefficient thermally corrected gravity anomaly inversion method of this embodiment includes the following steps:

[0061] a. Calculation of lithospheric thermogravity anomalies

[0062] According to the collected ocean magnetic anomaly data, the magnetic stripes are identified, and the ocean age isochrone is inferred, or the lithospheric thermal equilibrium time t can be obtained by referring to the existing ocean age isochrone data:

[0063] According to the measured seabed heat flow data, calculate the model thermal disturbance temperature T z :

[0064] T z = 2 T m π Σ n = 1 ∞ ( - 1 ...

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Abstract

The invention discloses a depth-varying-to-density earth crust expansion coefficient thermal calibration gravity anomaly retrieval method. In the calculation process of a gravity retrieval earth crust expansion coefficient, a lithosphere thermal gravity anomaly calibration and depth constraint strategy is introduced, according to an iterative computation method of multiple parameter constraints such as a submarine topography, a sedimentary thickness, magnetic anomaly, an ocean age isochron and earthquake reflection and refraction, a distortion effect, caused by earth crust density changes resulted from lithosphere thermal disturbance, on gravity interpretation is corrected, and a basis is provided for knowing earth crust expansion and cracking processes.

Description

Technical field: [0001] The invention relates to the field of earth sciences, in particular to a depth-variable-density crustal extension coefficient heat-corrected gravity anomaly inversion method. Background technique: [0002] Glossary: [0003] Stretch factor : is the coefficient of the extension degree of the crust of the extensional basin. McKenzie (1978) proposed the uniform stretching model of the lithosphere, also known as the pure shear model, which describes the basic response of the lithosphere to stretching, and defines the stretching coefficient β=l / b, where l is the stretching The lithosphere width, b is the initial width, which is used to describe the extension and thinning degree of the crust. Near the ocean-continental boundary (COB) or near the spreading axis of oceanic ridges, the extension of the continental lithosphere varies in depth, and the amount of extension increases with depth. [0004] heat correction : During the stretching and thinning p...

Claims

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Application Information

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IPC IPC(8): G01V1/36
Inventor 邱宁孙珍周蒂
Owner SOUTH CHINA SEA INST OF OCEANOLOGY - CHINESE ACAD OF SCI
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