This paper discusses hydrocarbon accumulation patterns of Moxizhuang oilfield of the Junggar Basin based on a comprehensive analysis of oilwater relationship
fault occurrence and hydrocarbon accumulation background.The reservoir of J
1
s
2(2)
(the lower second member of the Jurassic Sangonghe Formation) in Moxizhuang oilfield has a uniform oilwater system with a normal instead of inverted oilwater relationship.Seismic attributes of intervals with welldeveloped coal beds reveals that the previously interpreted major faults are artifacts resulted from seismic reflection of the coal seams
and no large faults are developed in the Sangonghe Formation
no faultsealing trap conditions exist.Hydrocarbon accumulation conditions and distribution characteristics are different inJ
1
s
2(1)
(the upper second member of the Jurassic Sangonghe Formation) and J
1
s
2(2)
reservoirs.The J
1
s
2(1)
reservoirs are developed in underwater distributary channel sandbodies of meandering river deltaic front facies
with the favorable reservoirs laterally being in strip distribution.In contrast
the J
1
s
2(2)
reservoirs are developed in distributary channel sandbodies of braided river delta facies
with the favorable reservoirs laterally in continuous distribution.The Moxizhuang oilfield is a structurallithologic reservoir that is controlled by both structure and sedimentary microfacies and is still in the posttilting dynamic adjusting process.There exists a uniform oilwater contact in J
1
s
2(2)
with occurrence the same as that of the updipping sandbody.