ON TOMOGRAPHY APPLYING IN THE THEKMAL CONDUCTIVITY VARIATION OF SEDIMENTARY FORMATIONS

Xue Aimin; Jiao lingxiu

doi:10.11781/sysydz199404397

Volume 16 Issue 4

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Article Navigation > PETROLEUM GEOLOGY & EXPERIMENT > 1994 > 16(4): 397-402

Xue Aimin, Jiao lingxiu. ON TOMOGRAPHY APPLYING IN THE THEKMAL CONDUCTIVITY VARIATION OF SEDIMENTARY FORMATIONS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1994, 16(4): 397-402. doi: 10.11781/sysydz199404397

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Xue Aimin, Jiao lingxiu. ON TOMOGRAPHY APPLYING IN THE THEKMAL CONDUCTIVITY VARIATION OF SEDIMENTARY FORMATIONS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1994, 16(4): 397-402. doi: 10.11781/sysydz199404397

Xue Aimin, Jiao lingxiu. ON TOMOGRAPHY APPLYING IN THE THEKMAL CONDUCTIVITY VARIATION OF SEDIMENTARY FORMATIONS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1994, 16(4): 397-402. doi: 10.11781/sysydz199404397

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ON TOMOGRAPHY APPLYING IN THE THEKMAL CONDUCTIVITY VARIATION OF SEDIMENTARY FORMATIONS

doi: 10.11781/sysydz199404397

Research Institute of Geophysics, Academia Sinica

Received Date: 1992-11-24
Publish Date: 1994-10-25

Abstract

Abstract

As the thermal conductivity of sedimentary formations is stable throughout the periodof sedimentary evoltition,it can be regarded as a constant. With a premise of invariable offluid property,the thermal conductivity of cemented rocks changes only with the variationof porosity and temperature,By the comptiter modellings on thermal history and sedimentary history,the thermal conductivity of rocks in different times can be inversed and imaged obtaining the images of thermal conductivity in varing times and depths, In this paper, the authors discuss the imaging method of thermal conductivity according to the fission track of apatite and the data of vitrinite reflectivity and suggest a theoretical model ofimaging using vitrinite reflectivity.

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References(5)

References

[1]	Andrews-Speed,Oxburgh ER and cooper BA.-Temperature and Depth-Dependent Heat Flow in Western North Sea,AAPG Bedlrtin 1984,68:1764-1781
[2]	Dave Deming and David Shapmans. Thermal Histories and Hydrocarbon Generation:Example form Utah-Wyoming Thruat BeIt.AAPG Bulletin,1989,73,1455-1471
[3]	Green PF. Duddy IR. Laslett GM.Hegarth KA.Gleadow AJW and Lowering JF. Thermal annealing of fission tracks in apatite 4. Quantitative modelling techniques and extension to geological timescales. Chemical Geology (Isotope Geoscience Section),1989.79,155-182
[4]	Lutz TM and Gomaa Omar. An inverse method of modelling thermal histories from apatite fission-track data.Earth and Planetary Science Lttttrs. 1991,104:181-185
[5]	Wood DA. Relationships Between Thermal maturity Indices Caculated Using Arrhenius Equation and Lopatin Method,Implications for Petrolum Exploration,AAPC Bnllrtin,1988.72.115-134

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ON TOMOGRAPHY APPLYING IN THE THEKMAL CONDUCTIVITY VARIATION OF SEDIMENTARY FORMATIONS

doi: 10.11781/sysydz199404397

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ON TOMOGRAPHY APPLYING IN THE THEKMAL CONDUCTIVITY VARIATION OF SEDIMENTARY FORMATIONS

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