Results 31 to 40 of about 2,052 (166)
Overpressure is an important phenomenon observed in sedimentary basins. To enhance the precision of identifying the origin of overpressure and predicting it accurately, this paper presents four practical methods for analyzing formation overpressure ...
Zeyang Xu +6 more
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In view of the difficulties in the study of lithofacies paleogeography and the low reliability of the distribution range of sedimentary sand bodies in the prototype basin caused by less deep drilling, complex seismic imaging and low degree of exploration
Zhiyong GAO +4 more
doaj +1 more source
The discovery of Carboniferous hydrocarbon source rocks in the Mahu-Shawan Sag has implied considerable exploration potential in the Carboniferous strata in the western Junggar Basin.
Shan Lu +15 more
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Supplementary Table 1. Petrographic, porosity and permeability data as well as depositional facies of the Lower Jurassic sandstones, central Junggar ...
Yong Il Lee (7909472) +1 more
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Tectono‐stratigraphic history of the southern Junggar basin: seismic profiling evidences [PDF]
AbstractThe modern Tianshan is an active intracontinental range in central Asia. Its initial timing is poorly known and still hotly debated. As the subsidence of foreland basins is intrinsically coupled with the uplift of orogenic wedges, the foreland sedimentary records may accurately constrain the Tianshan uplifting history.
Wang, Shengli +4 more
openaire +3 more sources
Malus sieversii, a wild progenitor of domesticated apple, is distributed in western Xinjiang of China, eastern part of Kazakhstan and Kyrgyzstan in Central Asia.
H. X. Zhang +5 more
core +1 more source
The basin type of the Junggar Basin changed during the Permian, but the time constraint of the tectonic evolution remains unclear. Besides, the fan deltas developed in the Permian in the Mahu Sag in the northwestern of the oil-rich basin.
Xingyu Chen +6 more
core +1 more source
A Magnetotelluric profile stretching northward from the Wulungu Depression (on the northern margin of the Junggar Basin) to the Dulate arc (crossing the Zhaheba–Aermantai ophiolite belt) was carried out in an attempt to probe the crustal structure and ...
Pingchuan Zhang +2 more
doaj +1 more source
In the Junggar Basin, northwestern China, the biostratigraphy and vegetation patterns of the MiddIe-Late Triassic sediments are comparativeIy poorly resolved.
Peng, Jungang +2 more
core +2 more sources
According to the distribution and transfer directions of thrust displacements under which the size, shape and pattern of thrust belt are controlled, the foreland thrust belts are classified into four types in middle and western China: (1) Type I, all the
Shuwei GUAN +3 more
doaj +1 more source

