Citation: | LIU Rong, MA Jian-qing, LI Qing-chun, YE Pei-sheng. GRAVITY, MAGNETIC AND ELECTRIC COMPREHENSIVE GEOPHYSICAL PROSPECTING FOR DEEP STRUCTURES IN HETAO BASIN[J]. Journal of Geomechanics, 2016, 22(4): 943-954. |
The gravity, magnetic, and electrical methods have been used to reveal the structure developed in the deep covered area of the Hetao Basin. We have carried out a lot of research on the characteristics of the northern and southern boundary faults, the features and thickness of Quaternary sediments and the structures developed in the basement of the Hetao Basin. A preliminary study on the distribution of Quaternary aquifer in this area was made by using electrical resistivity method. The joint inversion results of gravity and magnetic data, and earthquake data have been analyzed. And four concealed fault F1 to F4 from south to north and Langshan-Seertengshan piedmont fault F5 have been revealed. The fluctuation and buried depth of the crystalline basement in the area have been revealed. Depth of the basement in the southern part of the study area is about 2.5~4.2 km, and which in the northern part is up to 6 km. North Adjacent to the Seertengshan piedmont fault, the basement rock has been uplifted to about 0-1 km.
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Structure outline of Hetao Basin and adjacent area
DEM of the Hetao Basin and location of the study area
The measured Bouguer gravity anomaly (Δg) compared with regional gravity anomaly in line 100-110-120
Measured Bouguer gravity anomaly profile of profite 130
Measured magnetic anomalies (ΔT) and aeromagnetic anomaly profile of profile 100-110-120
Ultra high density inversion section in arrangement of 45-44
Super high density inversion in section 33-36 of the 100 cross section
Super high density inversion section in arrangement 37-100 of 110 section
AMT resistivity inversion model from point 110 in line 110
Fitting curves of gravity and magnetic inversion
The deep model of the covered area in Hetao Basin