 Posted: Mon 21:31, 14 Feb 2011 Post subject: Thermal infrared remote sensing in the Ordos Plate |
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| Thermal infrared remote sensing geological structures buried in the Ordos Plateau
That old basement uplift, faults cut by east-west (Figure 9,10), which is the same as thermal infrared remote sensing interpretation. East of gravity and magnetic anomalies for the North East to the zonal distribution,moncler uomo, interpreted as Yulin uplift, the eastern edge of the narrow gradient zone is a reflection of the basement faults, but also with the same interpretation of thermal infrared remote sensing. Thermal infrared remote sensing of a big puddle on the map Suide fault zone in the gravity and magnetic anomaly map was no response, the past has rarely mentioned in this tectonic zone, l994 in a formal setting such as Mr. Zhang Fuli side of things to construct a wubu , and thermal infrared remote sensing images are displayed on a large puddle with a consistent fault Suide - West Uplift Mu gravity and magnetic anomaly map is no clear indication. NE a Etuoke Banner Hangjinqi fault bundle in the past has not reported, gravity and magnetic anomaly map clearly shows that no. Mr. Teng Jiwen recent analysis of seismic waves that crustal uplift in the Ordos region. Under normal circumstances, the depression basin is wide and slow with the central station this interpretation is consistent syncline. Seismic analysis also pointed out that the mountain, under the Yellow River at the junction of Shaanxi is a north-northeast trending deep faults, and thermal infrared remote sensing temperature map JIAXIAN seen to the north of the north-northeast fault zone agreement. * 32 * Geophysics May 1996 Figure Head Basin residual gravity anomaly and aeromagnetic anomalies, magnetic body hot stack of Tanzania sets the minimum figure (according to Zhang Kang 1989) 1 Hangsheng �� _r positive anomaly; 2. Residual gravity high: 3. Sheng, bulk least buried thrust Field on the Anglo play and nose uplift; 4 - Sheng, bulk minimum buried Exploration; fields lower than the elevation of a 5ooom the region's first u No. 2 Gebi as other t thermal infrared remote sensing Ordos plateau concealed quality of play made her '33 'Figure lO from the top surface of Ordos Basin bedrock excellent map (according to the Changqing Petroleum Council 1995) * 34 * Geophysics May 1996 8 Conclusion temperature independent thermal infrared spectral index is calculated , surface emissivity calculation method makes the window can calculate thermal infrared surface temperature remote sensing data, of the principles of evidence-based thermal infrared remote sensing graph interpretation of the Quaternary buried under overburden geological structure,GHD glätteisen online shop, this new approach different from traditional underground geological geophysical methods, in time, manpower, funding and detection area has advantages, the future need to constantly improve, and promote the application. Comparison of thermal infrared remote sensing temperature map fast and continuous display a wide range of Quaternary tectonic pattern t is useful for mineral exploration in the symbol table should be thrown during the day and night thermal infrared map, it also shows the surface Yonghe The distribution of shallow groundwater. Geothermal resources also can reveal the distribution of drift. Reference. Zhang Fu Zha and other literature C13 test,moncler 2011, Juan Ordos Basin Gas Geology, 1994, Geological Publishing House. [2] Zhang Kang. Making and resources in Ordos decapitated orange, 1989, Shaanxi Science and Technology Press. [3] GUO stuffing, etc.,p90x workout calendar, oil and gas basins of northwest China and the outer ring data evaluation summary report. 1985. Changqing Petroleum Exploration Bureau. [4] garlic,timberland portugal, the scent of ink and so on. North geothermal. 1988. Science Press. [5) Wang Weiyong and so on. Geothermal basic theoretical research. 1982. Geological Publishing House. THERMALFRAREDREM0TESENSGHmDENsTRUCTURE0FEERDU0SIPLATEAUGeBiruTengJiwen (Ir ~ sfitute. FGeophyNcs, Academi ~ S ~ nieaBeljing100101) ZhengXinjiangLuWenjieGengShumin (N b ti mouth MeteorologicNSatellitl ~ CenterBeijing100081) AbactCalculatthelandsurfacetemperaturefieldwiththermalchannehdateofNOAA a 11flrat �� thenknterpretthisfieldaeenrdinga8thermaleonduefivityandradiogenicheatrateofroehs, 30thatrec0gveregionalhiddenstrueturaleunder-quaternary. KeyWordsThermal ~ nfraredr ~ rnotesenMnghiddenstructuralland music ect ~ tperattirefield |
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