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- W2128571200 abstract "Thermal indicator tomography is a new approach in determining the geological parameters by using nonlinear inverse methods. The essence of thermal indicator tomography is to (1) construct a model that approximates past thermal behavior in the subsurface, (2) compute theoretical thermal indicators to each sedimentary layer by forward tracing in time through the model, (3) measure the actual thermal indicators from the appropriate depths and then modify the thermal model through which the theoretical thermal indicators traveled in time to minimize the difference between measured and computed maturations. The process is nonlinearly updated until a preassigned degree of mismatch is obtained. To illustrate thermal indicator tomography, vitrinite reflectance with depth, /sup 39/Ar//sup 40/Ar ratio, sterane and hopane isomerization, and sterane aromatization were chosen as thermal indicators to determine simultaneously several geologic parameters such as erosion at unconformities, the timing of listric faulting, emplacement of igneous intrusions, the time and depth location of paleo-overpressure, and the age for a stratigraphic horizon." @default.
- W2128571200 created "2016-06-24" @default.
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- W2128571200 date "1988-01-01" @default.
- W2128571200 modified "2023-09-25" @default.
- W2128571200 title "Thermal Indicator Tomography--A New Approach to Determination of Geological Parameters: ABSTRACT" @default.
- W2128571200 doi "https://doi.org/10.1306/703c879a-1707-11d7-8645000102c1865d" @default.
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