In order to study the relationship of energy mineral deposits and tectonic movements in Ordos basin, more than 82 samples were taken for determination of apatite and zircon fission tracks. Furthermore, 93 apatite and zircon fission tracks have been selected from other publications. According to these data and other geological background, the evolution of Ordos basin can be divided into 4 stages, and the reformation of the basin can be divided into 5 stages. The basin formation and development were controlled by regional geodynamics. Oil, coal, nature gas and uranium deposits were formed in deferent stages. In the same time, 140 samples were taken and analyzed by organic and inorganic geochemical methods. The results indicate that coal and source rocks generate oil and natural gas, which migrate through reservoir rocks. Oil and natural gas changed the redox conditions of sediments and let uranium accumulate in the sandstones.
BeitlerB.ChanM. and ParryW., 2003. Bleaching of Jurassic Navajo Sandstone on Colorado Plateau Laramide highs: Evidence of exhumed hydrocarbon supergiants?Geology31(12), 1041–1044.
2.
ChenF.Z., 2002. Hydrogeology and uranium forming prospects in the north part of the Ordos Basin. Uranium Geology18, 287–294.
3.
DaiS.F.AiT.J.JiaoF.L.MaF.X. and LiB.C., 2000. Components of sulfur isotopes and characteristics of sulfur evolution in Wuda Coalfield, Inner Mongolia. Acta Petrologica Sinica16(2), 269–274 (in Chinese with English abstract).
4.
DaiS.F.RenD.Y.ChouC.L.LiS.S. and JiangY.F., 2006. Mineralogy and geochemistry of the No. 6 coal (Pennsylvanian) in the Junger Coalfield, Ordos Basin, China. International Journal of Coal Geology66, 253–270.
5.
DaiS.F.RenD.Y.SunY.Z. and TangY.G., 2004. Concentration and sequential chemical extraction procedures of U and Th in the Paleozoic coals from the Ordos Basin. Jounal of China Coal Society29 (Sup.), 56–60 (in Chinese with English abstract).
6.
DiY.Q., 2002. The prospects of uranium deposits in the Mesozoic and Cenozoic from the north part of the Ordos Basin. Uranium Geology18, 340–347 (in Chinese).
7.
FengZ.Z.BaoZ.D. and KangQ.F., 1999. Palaeotectonic of the Ordos Basin in the Palaeozoic. Journal of Palaeography1, 84–90 (in Chinese with English abstract).
8.
QiaoFengXiaoliZhangYunpingWangAipingFan and YiqunLiu, 2006. Characteristics of migration and accumulation of hydrocarbon and its deposit-formation signification in Upper Paleozoic in North Ordos basin. Acta Geologica Sinica80, 748–752 (in Chinese with English abstract).
9.
JiaJ.D.HeG.Q. and LiM.S., 1997. Base rocks and structures of the Ordos Basin. Journal of geology of universities3, 144–153 (in Chinese with English abstract).
10.
LiuC.Y.ZhaoH.G.GuiX.J.WangF. and ChenH., 2005. Attributes of the Mesozoic Structure on the West Margin of the Ordos Basin. Acta Geologica Sinica80, 1–38 (in Chinese with English abstract).
11.
LiuC.Y.ZhaoH.G.GuiX.J.YueL.P.ZhaoJ.F. and WangJ.Q., 2006. Space-time coordinate of the evolution and reformation and mineralization response in Ordos basin. Acta Geologica Sinica79, 738–747 (in Chinese with English abstract).
12.
PuR.H., 2000. The role and significances of paleotectonics in the nature gas formation in Ordos Basin. Nature Gas Industry104, 27–29.
13.
RadkeM.WillschH.LeythaeuserD. and TeichmüllerM., 1982. Aromatic components of coal: Relation of distribution pattern to rank. Geochim. Cosmochim. Acta46, 1831–1848.
14.
RadkeM. and WelteD. H. (1983) The methylphenenanthrene Index (MPI): A maturity parameter based on aromatic hydrocarbons. In: BjoroyM. (Ed.), Advance in Organic Geochemistry 1981, pp. 504–512. Wiley, Chichester.
15.
RenZ.L., 1995. Thermal history of Ordos basin by apatite fission track analysis. Acta Geophysica Sinica38(3), 339–349 (in Chinese with English abstract).
16.
ZhanliRenShengZhangShengliGaoJunpingCui and XinsheLiu, 2006. Reasearch on region of maturation anomaly and formation time in Ordos basin. Acta Geologica Sinica80, 674–684 (in Chinese with English abstract).
17.
SunY.Z.SunJ.P.ZhangH.J. and LiuL.F., 2002. Recovery of origin organic parameters of the samples from the outcropping source rocks in the Shiwanshan Basin, Southern China. Energy Exploration and Exploitation20(5)365–370.
18.
SunY.Z.ChenJ.P.LiaoW.LuJ.L. and ZhangH.J., 2004. Formation and distribution of polycyclic aromatic sulfur compounds in the Kupferschiefer from Poland and Germany. World Journal of Engineering1(2), 74–92.
19.
SunG.F., 1981. The formation and development of the Ordos Basin. Collections of petroleum geology, Geology Publishing, Beijing.
20.
WangS.M., 1996. Coal accumulation and evolution of the coal resource in the Ordos Basin. Coal Industry Publishing, Beijing. pp. 437.
YangJ.J., 2002. Tectonic Evolution of Ordos Basin and Distribution Regularities of Petroleum and Natural Gas. Petroleum Industry Publishing, Beijing. pp. 73–74; 86–88.
23.
YangJ.J. and ZhangB.R., 1990. The main features of over-thrust faults in western Ordos Basin. In: YangJ.J. (Ed.), Petroleum and over-thrust faults in western Ordos Basin. Gansu Science Publishing, Lanzhou. 91–105.
24.
ZhangG.W.ZhangB.R.YuanX.C. and XiaoQ.H., 2001Qinling Tectonic Belt and Continental Mechenism. Science Publishing, Beijing. pp. 706–724.
25.
ZhangH.HeZ.L. and JinX.L., 2005. Tectonic Evolution of Ordos Basin and Coal Formation. Introduction for 1:500000 Geological Map of Ordos Basin. Geological Publishing, Beijing. pp. 49–58.
26.
ZhangW.Z., 1999. The geologic characters of large petroleum and gas reservoirs in the Ordos Basin. Marine petroleum geology of China13, 391–394.
27.
ZhaoC.Y., 1990. Evolution of western margin of Ordos Basin and its plate geodynamic mechanisms. Northwest University Publishing, Xi'an. pp. 107–114.
28.
ZhaoM.W.HansJ.B. and HansA., 1996. Thermal and Tectonic History of the Ordos Basin, China: Evidence from Apatite Fission Track Analysis Vitrinite Reflectance, and K-Ar Dating. AAPG Bulletin80, 1110–1134.
29.
ZhouZ.Y.GuoT.L.XuC.H. and YangF.L., 2005. Fission Track Analysis on Mesozoic Strata in the Shiwandashan Basin, Guangxi Province and its geological significance. Acta Geologica Sinica79, 395–401 (in Chinese with English abstract).
