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沉积学报 1986
THEPARAMAGNETICRESONANCEANDCARBONISOTOPEFEATURESOFTHECRUDEOILANDSOURCEROCKSINZHUNGEERBASIN, PP. 9-18 Abstract: ThesedimentaryareaofZhungeerBasinisabout130,000km2anditssedimentaryrocksfromCarboniferoustillLatterTertiaryare2,000minmaximumthickness.Owingtothelong一termandstablesinkingdominatingoverthebasinandtheinflueneeoftherift一differentialmovementinthebasin,different011一formingdepressionswereformedindifferentgeologiealperiods.
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