The Junggar basin of northwestern China is a structural basin containing a thick sequence of Paleozoic-Pleistocene rocks with estimated oil reserves of as much as 5 billion bbl. Protected against the penetration of cold northern winds, the basin is much warmer in the winter than are the more southerly plains of southeast China. Lucky You! Introduction In arid and semi-arid areas, water resources are the major factor limiting crop yields [1]. The 2-D wide-angle reflection/refraction seismic profile OBS2006-2 is almost parallel to the extinct spreading ridge (ESR) of the NWSB. Analyses of 19 oil samples from nine producing fields and two oil-stained cores in the Junggar basin revealed the presence of at least five genetic oil types. In this study, we aimed to understand the growth dynamics of the region, to forecast its future expansion, and to provide a basis for regional management. Except for the Chengdu Plain, the region is hilly. Junggar Basin is one of the largest sedimentary basins in Northwest China.It is located in Xinjiang, and enclosed by the Tarbagatai Mountains of Kazakhstan on the northwest side, the Altai Mountains of Mongolia in the northeast, and the Heavenly Mountains (Tian Shan) in the south. Basin, Donetsk Basin and Britain; Lochengia migrated easterly to South China and westerly to the Urals seaway and the adjoined Russian Platform (i.e., both the Moscow and Donetsk Basins). The Sichuan Basin is surrounded by mountains, which are higher in the west and north. The middle basin of Heihe River has witnessed rapid urban growth and excessive agricultural activities during the last two decades, mainly because of its economic development and increasing population pressure. The geology of Junggar Basin mainly consists of sedimentary rocks underlain by igneous and metamorphic basement rocks. Keywords: inland river basin; irrigation e ciency; Northwest China; water management 1. The deep crustal structure of the Northwest Sub-basin (NWSB) of the South China Sea (SCS) is of great importance for understanding the tectonic nature of the continent-ocean transition (COT) and magmatism in this oceanic basin. Striving for the right answers? Contemporary occupants of the Tarim Basin, a geographical area in the Xinjiang Uyghur autonomous region of northwest China, are both biologically and culturally diverse. The Kuqa foreland basin (KFB), north of the Tibetan Plateau, located between the Tarim Craton and the Tianshan Mountain in northwest China, is a Cenozoic salt-bearing basin with great hydrocarbon potential (Jia and Wei, 2002; Wang et al., 2013). The arid and semi-arid area occupies 52.5% of China’s land area, which is mainly distributed in Northwest, Northeast, and North China. China - China - The Sichuan Basin: This is one of the most attractive geographical regions of China. 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