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准噶尔

  • na.Sungar
  • 网络junggar; Dzungaria; jungar

准噶尔准噶尔
英-汉网络释义

准噶尔

na.

1.Sungar

例句：
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The south of Junggar basin has complicated structure , many entrapments and active surface, all this indicates a large resource quantity.
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The basement structure and property of the Junggar basin has long been a focus for geoscientists.
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The Yongjin Oilfield had been explored to be a large oilfield with in-place volume of hundreds millions ton in Junggar Basin.
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The Kebai fault zone is one of most prolific areas in Junggar Basin. But its oil source is still poorly understood.
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A typical foreland basin was formed at the front of Kalatnayli mountain, northeastern margin of Junggar basin.
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The Bogda Mountain, with Junggar basin on the north and Turpan-Hami basin on the south, is a part of the East Tianshan Mountains.
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Furthermore, these techniques have been proved reasonable and advanced when they applied to the south edge of Junngar Basin.
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Foreland fold-and-thrust belt in the southern margin of the Junggar basin is a product of the north Tianshan compression.
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There still exist some different opinions concerning the evolution of Junggar basin, an important oil-bearing basin in western China.
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The over- pressure system in Hutubi area of Junggar was benefit for the formation and conservation of gas pools.
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The tectonic evolution and hydrocarbon accumulation in the foreland fold-and-thrust belt of the southern JunggarBasin is complex.
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The Permian-Jurassic alluvial-fan, subaqua-fan and delta-fan were widely distributed in the west-north margin of Junggar Basin.
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The resolution of seismic data was low in Shinan Area of Jungar Basin, it could not satisfy the demands of lithologic reservoir exploration.
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Eastern section of Bogda orogenic belt is near the East Junggar orogenic belt.
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The Kalmyks migrated from Dzungaria to the southeastern European part of the Russian Federation nearly 400 years ago.
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are three early spring ephemeral plants of Brassicaceae which are common in Junggar Desert, Xinjiang.
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The distribution of oil and gas complex, multi-reservoir type in Hongche fault belt of the northwestern margin in Junggar Basin.
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The Qiangtang basin is one large Paleozoic-Cenozoic basin besides the Tarim, Qaidam and Junggar basins in western China.
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The main reservoir of Jurassic Badaowan Formation at Wuxia area is composed of sand bodies of alluvial fan and braided river.
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The physical and geochemical properties of viscous oil in the northwest margin ofJunggarBasin were studied in the paper.
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