It is proved from the data of seismic,well logging and core data that the deposit of deltic subwater distributary channel developed in East 3 member of Dongying Formation in Xianhe area of Liaohe shore,which is made of sandy conglomerates or gravel-bearing sandstones according to the core data,showing high value clock-shaped curve in the well logging and high amplitude lens-shaped reflection in the seismic section.
Among the Chang-6 oil-bearing beds, the Chang-64 is delta-front facies, which is characterized by the connected distribution of subaqueous distributary channels.
With above all being combined with the analyses of the log data of sedimentary facies of several hundreds of wells and the grain-size distribution figures of tens of wells, it can be concluded that the sand bodies of Chang 6 oil-bearing strata in the study area are mainly distributary channel deposits of delta plain facies and delta front facies.
The deposits of braided river deltas are mainly composed of pebbled sandstone and medium to coarse grained sandstones. The bars of the subaqueous distributary channels are the main bodies of deltas. A single channel bar has a thickness of 0.5m 2.5m.
It is proposed firstly that the upper Permian in the southeast edge of Tazhong area is braidedstream delta deposit and its host is submerged distributary channel composed of conglomeratic sand and sandstone.
this pool belongs to delta front sub-facies sedimentary model, the underwater distributary channel and mouth bar is the better sedimentary microfacies;
Among the Chang-6 oil-bearing beds, the Chang-64 is delta-front facies, which is characterized by the connected distribution of subaqueous distributary channels.
Mainly consisting of sandstones and pebbled sandstones with minor siltstone and mudstone partings, the lower Lower Jurassic Abe Formation in Kuche depression is subaqueous distributary channel deposit of braided delta. In Ahe Formation there developed a kind of large scale cross-bedding, which is characterised by an average set thick of 0.5 to 2 m, frequently occuring reverse dip bedding of adjacent sets, repeatedly and alternately changing of dip directions vertically Through detained observation of 7 sect...
Being influenced by Landei Fracture of Triassic in Lunnan area, the elevations in the both sides on the fracture are large enough to make the alluvial fan to enter directly the lacustrine basin and to form the tan delta group deposition.The fan deltaic body can be divided into three subfacies,named fan delta plain,fan delta front and pro-fan delta.Subaquous distributary channel sand bodies in the fan delta front are most important reservoir of oil and gas. The developing area of reseroir is located at Sang...
A braided river system progrdes into a inland lake and forms a braidedriver delta.The deltas are very abundant in the Triassic system of Kuche depression,Tarim Basin.They are significantly different from the other types of deltas in the geomorphic and sedimentological setting.The coarse deposits of the braided channel and of the subaqueous distributary channel,mainly composed of pobbed sandstones and sandstones displaying finer-upward sequences in general,constitute the main body of the deltas.A single fine...