| Institute of Geomechanics, Chinese Academy of Geological Sciences | Host |
| Citation: |
LAO Hai-gang, WU Kong-you, CHEN Qing-hua. GEOLOGIC CHARACTER AND EVOLUTION OF THE ACCOMMODATION ZONE IN THE JIZHONG DEPRESSION[J]. Journal of Geomechanics, 2010, 16(3): 294-309.
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GEOLOGIC CHARACTER AND EVOLUTION OF THE ACCOMMODATION ZONE IN THE JIZHONG DEPRESSION
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Abstract
According to the accommodation structure theory, in combination with the analysis on geological map and paleo-fall, five accommodation zones and seven structure forms have be recognized in Jizhong Depression.The synthetic approaching-type accommodation zone can occur as nose structure, horst and transform fault, e.g., it occurs as nose structure exist in fault segment joints, but as coexistence of transform fault and transverse salient in the joints of faults controlling depression.The synthetic overlap-type accommodation zone transfers strain in the form of trend slope.The synthetic collateral-type accommodation zone reforms the Hexiwu buried hill belt in the form of warping.The convergent collateral-type accommodation zone develops in Yanling area in the form of low uplift.The convergent approaching-type accommodation zone, typically observed in the Maozhou hub zone, forms double-layer deformation system, which comprises a bottom of fault bifurcation oblique slip and an upper of wide cup zone.In the geological evolution, a relation of ebb and flow can be obserbed among the activity intensities of the faults which play the part of accommodation.With the effect and reformation of accommodation zone, a migration path for oil and gas, with ancient structural ridge as dominant migration pathway, can be formed on the slop of buried hill.
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References
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LAO Hai-gang, WU Kong-you, CHEN Qing-hua. GEOLOGIC CHARACTER AND EVOLUTION OF THE ACCOMMODATION ZONE IN THE JIZHONG DEPRESSION[J]. Journal of Geomechanics, 2010, 16(3): 294-309.
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Figure 1.
A map showing distribution of basement faults and accommodation structures in Jozhing Depression
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Figure 2.
Structural map showing Tertiary bottom boundary(Tg)in central Jizhong Depression
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Figure 3.
Basement faults and accommodation zones in northern Jozhing Depression
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Figure 4.
Seismic section on the horst-type transverse salient accommodation zone around Tongbai Town
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Figure 5.
Structural map showing Tertiary bottom boundary (Tg) in Suqiao-Yangcun area
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Figure 6.
The deposition environment diagram of Sha 3stage in Jizhong Depression[30]
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Figure 7.
Seismic section in the Yanling buried hill zone (through 6470 survey line)
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Figure 8.
The motion trace of the faults which produce the synthetic approaching-type accommodation zone in different period
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Figure 9.
The motion trace of the faults which produces the synthetic overlap-type accommodation zone in different periods
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Figure 10.
The motion trace of the faults which produces the synthetic collateral-type accommodation zone in different periods
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Figure 11.
The motion trace of the faults which produce the convergent collateral-type accommodation zone in different period
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Figure 12.
The motion trace of the faults which produce the convergent approaching-type accommodation zone in different periods
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Figure 13.
Tg structural map in fault ramp of Renqiu buried hill (dashed line is the extension direction of structure ridge, the circle is fault nose of Maxi)